Relevant bibliographies by topics / Geological mapping/Maseno area

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Geological mapping/Maseno area'

Author: Grafiati
Published: 4 June 2021
Last updated: 5 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Geological mapping/Maseno area.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Geological mapping/Maseno area"

1

Kotsanis, D., P. Panagiotopoulos, D. Rozos, and C. Loupasakis. "Engineering geological mapping of the Pallini urban area." Bulletin of the Geological Society of Greece 47, no. 4 (2013): 1715. http://dx.doi.org/10.12681/bgsg.11036.

Full text
Abstract:
Engineering geological thematic maps can provide substantial information for the development of cities, the land planning of future infrastructures and even more for the planning of the natural hazards prevention and/or mitigation. To this direction the engineering geological map of the Municipality of Pallini, at the Eastern Attica prefecture, at a scale of 1:20.000, was compiled. For that purpose, the following workflow was adopted: Firstly, a desk study helped in selecting the relevant topographic and geologic maps, which were digitized and introduced in a GIS environment. Secondly, the data coming from detailed geological mapping were elaborated to the same GIS environment. Thirdly, geotechnical data collected from borehole logs, such as lithostromatographic sequence, in situ tests and laboratory tests were introduced in geotechnical database. The statistical evaluation of this data provided estimates for numerous geotechnical parameters. Finally, the engineering geological map was compiled by merging the geological formations into lithologic units according to their origin, age, natural condition, and geotechnical characteristics.
APA, Harvard, Vancouver, ISO, and other styles
2

ARAI, Kohsaku, Gen SHIMODA, and Ken IKEHARA. "Marine geological mapping project in the Okinawa area." Synthesiology 6, no. 3 (2013): 162–69. http://dx.doi.org/10.5571/synth.6.162.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

ARAI, Kohsaku, Gen SHIMODA, and Ken IKEHARA. "Marine geological mapping project in the Okinawa area." Synthesiology English edition 6, no. 3 (2013): 158–65. http://dx.doi.org/10.5571/syntheng.6.158.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Asfahani, Jamal. "Characterization of Ar-Rassafeh Badyieh area (Area-2), Syria by using the airborne gamma-ray spectrometric and fractal modelling techniques." Contributions to Geophysics and Geodesy 49, no. 4 (2019): 459–78. http://dx.doi.org/10.2478/congeo-2019-0024.

Full text
Abstract:
Abstract The available aerial gamma-ray spectrometric data of Ar-Rassafeh Badyieh area (Area-2) are used herein for geological interpretations and mapping purposes. Those data are interpreted by the concentration-number (C-N) fractal modelling technique, with the use of log-log graphs. According to C-N model, different radioactive ranges of TC, eU, eTh, and K have been isolated. Those ranges are thereafter used to characterize the lithological outcrops in the study area. The radioactive signatures of all the outcrops in Area-2 have been discussed and documented through establishing the C-N maps of TC, eU, eTh, and K, and benefiting of the available geological map. The C-N fractal modelling technique proves its efficacy, where radioactive and lithological boundaries of outcrops are in concordance. The case study presented in this paper shows the importance and the role of airborne gamma-ray spectrometric and fractal modelling techniques to support the geological mapping and the interpretations in geological context, particularly when the study region is rugged and difficult to be accessed.
APA, Harvard, Vancouver, ISO, and other styles
5

Georgiadis, G. A., M. D. Tranos, Th K. Makedon, and G. Ch Dimopoulos. "Contribution of geological mapping in road construction: an example from Verta - Kozani National road, Kastania area." Bulletin of the Geological Society of Greece 40, no. 4 (2007): 1652. http://dx.doi.org/10.12681/bgsg.17069.

Full text
Abstract:
Road construction is a complex and multipart work that is decisively depended on the geological investigation of the area of interest. The geological investigation, which ought to be carried out from the early stages of the study and construction, contributes significantly in the cost reduction and corresponding increase of the construction safety. The proposed methodology that should be implemented during the geological investigation for this kind of constructions includes geological mapping and construction of geological and engineering geological maps. These maps display, in each case, the necessary data and are supplemented by geological crosssections as well as stereographic projections (e.g. Schmidt diagrams), which evaluate the tectonic conditions of the area and the stability conditions of artificial road slopes. An example of geological investigation based on the above methodology is presented, regarding the Kastania section of the Veria - Kozani (old) national road.
APA, Harvard, Vancouver, ISO, and other styles
6

Harvey, A. S., and G. Fotopoulos. "GEOLOGICAL MAPPING USING MACHINE LEARNING ALGORITHMS." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B8 (June 23, 2016): 423–30. http://dx.doi.org/10.5194/isprsarchives-xli-b8-423-2016.

Full text
Abstract:
Remotely sensed spectral imagery, geophysical (magnetic and gravity), and geodetic (elevation) data are useful in a variety of Earth science applications such as environmental monitoring and mineral exploration. Using these data with Machine Learning Algorithms (MLA), which are widely used in image analysis and statistical pattern recognition applications, may enhance preliminary geological mapping and interpretation. This approach contributes towards a rapid and objective means of geological mapping in contrast to conventional field expedition techniques. In this study, four supervised MLAs (naïve Bayes, k-nearest neighbour, random forest, and support vector machines) are compared in order to assess their performance for correctly identifying geological rocktypes in an area with complete ground validation information. Geological maps of the Sudbury region are used for calibration and validation. Percent of correct classifications was used as indicators of performance. Results show that random forest is the best approach. As expected, MLA performance improves with more calibration clusters, i.e. a more uniform distribution of calibration data over the study region. Performance is generally low, though geological trends that correspond to a ground validation map are visualized. Low performance may be the result of poor spectral images of bare rock which can be covered by vegetation or water. The distribution of calibration clusters and MLA input parameters affect the performance of the MLAs. Generally, performance improves with more uniform sampling, though this increases required computational effort and time. With the achievable performance levels in this study, the technique is useful in identifying regions of interest and identifying general rocktype trends. In particular, phase I geological site investigations will benefit from this approach and lead to the selection of sites for advanced surveys.
APA, Harvard, Vancouver, ISO, and other styles
7

Harvey, A. S., and G. Fotopoulos. "GEOLOGICAL MAPPING USING MACHINE LEARNING ALGORITHMS." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B8 (June 23, 2016): 423–30. http://dx.doi.org/10.5194/isprs-archives-xli-b8-423-2016.

Full text
Abstract:
Remotely sensed spectral imagery, geophysical (magnetic and gravity), and geodetic (elevation) data are useful in a variety of Earth science applications such as environmental monitoring and mineral exploration. Using these data with Machine Learning Algorithms (MLA), which are widely used in image analysis and statistical pattern recognition applications, may enhance preliminary geological mapping and interpretation. This approach contributes towards a rapid and objective means of geological mapping in contrast to conventional field expedition techniques. In this study, four supervised MLAs (naïve Bayes, k-nearest neighbour, random forest, and support vector machines) are compared in order to assess their performance for correctly identifying geological rocktypes in an area with complete ground validation information. Geological maps of the Sudbury region are used for calibration and validation. Percent of correct classifications was used as indicators of performance. Results show that random forest is the best approach. As expected, MLA performance improves with more calibration clusters, i.e. a more uniform distribution of calibration data over the study region. Performance is generally low, though geological trends that correspond to a ground validation map are visualized. Low performance may be the result of poor spectral images of bare rock which can be covered by vegetation or water. The distribution of calibration clusters and MLA input parameters affect the performance of the MLAs. Generally, performance improves with more uniform sampling, though this increases required computational effort and time. With the achievable performance levels in this study, the technique is useful in identifying regions of interest and identifying general rocktype trends. In particular, phase I geological site investigations will benefit from this approach and lead to the selection of sites for advanced surveys.
APA, Harvard, Vancouver, ISO, and other styles
8

Karageorgiou, M. M. D., E. Karymbalis, and D. E. Karageorgiou. "THE USE OF THE GEOGRAPHICAL INFORMATION SYSTEMS (G.I.S) IN THE GEOLOGICAL – MINERALOGICAL MAPPING OF THE PARANESTI AREA." Bulletin of the Geological Society of Greece 43, no. 3 (2017): 1601. http://dx.doi.org/10.12681/bgsg.11334.

Full text
Abstract:
The aim of this study is to emphasize the role of the Geographical Information Systems (GIS) technology for the collection, organization, analysis, modeling and presentation of data required for the geological and ore-deposits mapping. As a case study area the region of Paranesti in Northern Greece was selected as it is of exceptional geological and uranium mining interest. For the geological and ore deposit mapping of the study area data derived from analogue maps at various scales (topographical and geological) along with detailed field geological observations and measurements were organized in a spatial database with a common geographical coordinate system utilizing GIS technology. This procedure revealed the relation between the geographical distribution of uranium deposits and the geological structure of the area as well as the effect of the active tectonics.
APA, Harvard, Vancouver, ISO, and other styles
9

Dandar, Otgonbayar, Atsushi Okamoto, Masaoki Uno, Undarmaa Batsaikhan, Burenjargal Ulziiburen, and Noriyoshi Tsuchiya. "Drone brings new advance of geological mapping in Mongolia: Opportunities and challenges." Mongolian Geoscientist, no. 47 (December 31, 2018): 53–57. http://dx.doi.org/10.5564/mgs.v0i47.1063.

Full text
Abstract:
Unmanned aerial vehicles (UAVs) or drones have revolutionized scientific research in multiple fields. Drones provide us multiple advantages over conventional geological mapping or high-altitude remote sensing methods, in which they allow us to acquire data more rapidly of inaccessible or risky outcrops, and can connect the spatial scale gap in mapping between manual field techniques and airborne, high-altitude remote sensing methods. Despite the decreased cost and technological developments of platforms, sensors and software, the use of drones for geological mapping in Mongolia has not yet been utilized. In this study, we present using of drone in two areas: the Chandman area in which eclogite is exposed and the Naran massif of the Khantaishir ophiolite in the Altai area. Drone yields images with high resolution that is reliable to use and reveals that it is possible to make better formulation of geological mapping. Our suggestion is that (1) Mongolian geoscientists are encouraged to add drones to their geologic toolboxes and (2) drone could open new advance of geological mapping in Mongolia in which geological map will be created in more effective and more detailed way combined with conventional geological survey on ground.
APA, Harvard, Vancouver, ISO, and other styles
10

Park, Gyesoon, Samgyu Park, Jeong-Sul Son, Changryol Kim, and Seong-Jun Cho. "Potential Mapping of Moisan area Using SIP and 3D Geological Modeling." Geophysics and Geophysical Exploration 17, no. 4 (2014): 209–15. http://dx.doi.org/10.7582/gge.2014.17.4.209.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Geological mapping/Maseno area"

1

Opiyo-Akech, Norbert. "Geology and geochemistry of the late Archaean greenstone associations, Maseno area, Kenya." Thesis, University of Leicester, 1988. http://hdl.handle.net/2381/35080.

Full text
Abstract:
The greenstone belt of Kenya is an extension of what is commonly referred to as the Tanganyika "Shield". The two supracrustal sequences recognized in Kenya are the Nyanzian and the Kavirondian. The rocks found in these sequences are diverse, with dominant volcanics in the Nyanzian, whereas the Kavirondian is predominantly sedimentary. The Nyanzian lavas represent a diverse range from basalts and basaltic andesites, through andesites and dacites to rhyolites. From geochemical studies the basalts and basaltic andesites are tholeiitic, whereas the andesites, dacites and rhyolites are calc-alkaline. The sedimentary sequence ranges from mudstone, through shales, sandstones and grits to conglomerates. The plutonic rocks range in composition from gabbro to true granites, but tonalite is the dominant rock type. The chemical differences between the tholeiitic basalts and the calc-alkaline andesitic to rhyolitic sequences suggests that these volcanic suites are derived from different sources and/or through different processes. The granitoids have close chemical similarities with the silicic volcanics. From the geochemical and field relationships, the Nyanzian and Kavirondian sequences are considered to have developed on a continental segment which had not yet attained full stability. The model employed for the generation of these volcanics considers the basalts to have been generated in a region undergoing extension, similar to that of a modern back-arc environment, whereas the calc-alkaline sequences, including the granitoids, are broadly comparable with those found in present day continental arc environments.
APA, Harvard, Vancouver, ISO, and other styles
2

Stephen, Tammie Debra. "Insights into mineralisation of the Luxemburg Mine Area, Olary, South Australia, from geological mapping, strain and microstructural analysis, and geophysics /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bs831.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Saunders, Peta J. "The structural evolution of the Bull Creek area, southern Adelaide fold belt, South Australia, through the integration of geological mapping and geophysical interpretation /." Title page, abstract and contents only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbs257.pdf.

Full text
Abstract:
Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1994.<br>Australian national grid reference: Milang (SI 54) 6627-II 1:50 000 sheet. Four maps have overlays. Includes bibliographical references.
APA, Harvard, Vancouver, ISO, and other styles
4

Perks, Matthew James. "The mid-crust of the western Slave Province, geological mapping, geochemistry, and U-Pb geochronology of the forked lake area, southwestern Slave Province, Northwest Territories." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/mq22653.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Zaine, José Eduardo. "Mapeamento geológico-geotécnico por meio do método do detalhamento progressivo : ensaio de aplicação na área urbana do município de Rio Claro (SP) /." Rio Claro : [s.n.], 2000. http://hdl.handle.net/11449/102900.

Full text
Abstract:
Orientador: Leandro Eugenio da Silva Cerri<br>Banca: Nilson Gandolfi<br>Banca: Antonio Manoel dos Santos Oliveira<br>Banca: Fábio Taioli<br>Banca: Omar Yasbek Bitar<br>Resumo: A pesquisa teve como tema central o mapeamento geológico-geotécnico de áreas urbanas, analisando os dados do meio físico geológico, bem como a representação cartográfica de unidades geotécnicas. O estudo envolveu a análise das metodologias utilizadas nos trabalhos de cartografia geotécnica, com enfoque especial para duas linhas metodológicas brasileiras, ou seja, as metodologias utilizadas pela Escola de Engenharia de São Carlos e pelo IPT. O trabalho apresenta o método do detalhamento progressivo como alternativa aos estudos geológico-geotécnicos, tendo como objetivo principal a produção de instrumentos adequados para a gestão e o planejamento urbanos, ante as necessidades de seus principais usuários. Tal método consiste na adoção de diferentes escalas de abordagem para a elaboração de cartas e/ou mapas geotécnicos, com o desenvolvimento dos trabalhos em três etapas sucessivas, em níveis de detalhe crescentes, do geral (1ª etapa) para o particular (etapa de detalhe). O ensaio de aplicação do método do detalhamento progressivo foi realizado numa área de 160 km2, envolvendo o sítio urbano e de expansão urbana de Rio Claro, uma cidade de médio porte, do interior paulista. A 1ª etapa mostrou que estudos geológicos e geomorfológicos são fundamentais para orientar as etapas subseqüentes; e a quantificação de alguns parâmetros na 2ª etapa foi importante para a melhor caracterização das unidades de estudo. A realização de ensaios de laboratórios na 3ª etapa é melhor dimensionada quando orientada pelas fases anteriores, estudos estes, efetivamente aplicados, se direcionados a projetos e obras.<br>Abstract: This paper's main theme is engineering geological mapping in urban areas, bringing together the results of the assembly, analysis and interpretation of geological data, as well as the cartographic representation of geotechnical units. As part of the study, an analysis of methodologies used in engenheering geological mapping was made, with special emphasis on two lines of Brazilian methodologies, i.e., the procedures used by the Engineering School of São Carlos - University of São Paulo and by the Institute of Technological Researches of the State of São Paulo S.A. - IPT. The main purpose of the study is to apply the progressive detailing method to engineering geological maps in urban areas, with a view to produce more adequate instruments for urban administration and planning, taking into consideration the necessity of the users. The progressive detailing method's application was made in a 160 km2 area that included an urban site and urban expansion in the municipal district of Rio Claro, a medium size town of the state of São Paulo, Brazil. The progressive detailing method consists of adopting different approach scales in engineering geological mapping, with the study being divided into three successive stages, in levels of increasing detail, from general to specific. The first stage showed the importance of geologic and geomorphologic studies on the development of next stages. The quantification of some parameters on 2nd stage was of great value on characterization of the units of study. The completion of laboratories analysis on the 3rd stage to subsidy projects and buildings, is better evaluated if it is guided for previous stages.<br>Doutor
APA, Harvard, Vancouver, ISO, and other styles
6

Zaine, José Eduardo [UNESP]. "Mapeamento geológico-geotécnico por meio do método do detalhamento progressivo: ensaio de aplicação na área urbana do município de Rio Claro (SP)." Universidade Estadual Paulista (UNESP), 2000. http://hdl.handle.net/11449/102900.

Full text
Abstract:
Made available in DSpace on 2014-06-11T19:32:18Z (GMT). No. of bitstreams: 0 Previous issue date: 2000-02-28Bitstream added on 2014-06-13T20:43:13Z : No. of bitstreams: 1 zaine_je_dr_rcla.pdf: 10722625 bytes, checksum: 58a2ea16d5ca5a5f98a15ce993e4b07b (MD5)<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>A pesquisa teve como tema central o mapeamento geológico-geotécnico de áreas urbanas, analisando os dados do meio físico geológico, bem como a representação cartográfica de unidades geotécnicas. O estudo envolveu a análise das metodologias utilizadas nos trabalhos de cartografia geotécnica, com enfoque especial para duas linhas metodológicas brasileiras, ou seja, as metodologias utilizadas pela Escola de Engenharia de São Carlos e pelo IPT. O trabalho apresenta o método do detalhamento progressivo como alternativa aos estudos geológico-geotécnicos, tendo como objetivo principal a produção de instrumentos adequados para a gestão e o planejamento urbanos, ante as necessidades de seus principais usuários. Tal método consiste na adoção de diferentes escalas de abordagem para a elaboração de cartas e/ou mapas geotécnicos, com o desenvolvimento dos trabalhos em três etapas sucessivas, em níveis de detalhe crescentes, do geral (1ª etapa) para o particular (etapa de detalhe). O ensaio de aplicação do método do detalhamento progressivo foi realizado numa área de 160 km2, envolvendo o sítio urbano e de expansão urbana de Rio Claro, uma cidade de médio porte, do interior paulista. A 1ª etapa mostrou que estudos geológicos e geomorfológicos são fundamentais para orientar as etapas subseqüentes; e a quantificação de alguns parâmetros na 2ª etapa foi importante para a melhor caracterização das unidades de estudo. A realização de ensaios de laboratórios na 3ª etapa é melhor dimensionada quando orientada pelas fases anteriores, estudos estes, efetivamente aplicados, se direcionados a projetos e obras.<br>This paper's main theme is engineering geological mapping in urban areas, bringing together the results of the assembly, analysis and interpretation of geological data, as well as the cartographic representation of geotechnical units. As part of the study, an analysis of methodologies used in engenheering geological mapping was made, with special emphasis on two lines of Brazilian methodologies, i.e., the procedures used by the Engineering School of São Carlos - University of São Paulo and by the Institute of Technological Researches of the State of São Paulo S.A. - IPT. The main purpose of the study is to apply the progressive detailing method to engineering geological maps in urban areas, with a view to produce more adequate instruments for urban administration and planning, taking into consideration the necessity of the users. The progressive detailing method's application was made in a 160 km2 area that included an urban site and urban expansion in the municipal district of Rio Claro, a medium size town of the state of São Paulo, Brazil. The progressive detailing method consists of adopting different approach scales in engineering geological mapping, with the study being divided into three successive stages, in levels of increasing detail, from general to specific. The first stage showed the importance of geologic and geomorphologic studies on the development of next stages. The quantification of some parameters on 2nd stage was of great value on characterization of the units of study. The completion of laboratories analysis on the 3rd stage to subsidy projects and buildings, is better evaluated if it is guided for previous stages.
APA, Harvard, Vancouver, ISO, and other styles
7

Teng, Chia-Hsin, and 鄧嘉欣. "Application of Airborne LiDAR on geological mapping –Case study of the Huanshan area." Thesis, 2015. http://ndltd.ncl.edu.tw/handle/uct8gy.

Full text
Abstract:
碩士<br>國立臺北科技大學<br>資源工程研究所<br>103<br>Whether looking for traditional geological mapping depend on continuous outcrop, topographic data (e.g. topographic map and Digital Terrain Molde), which is located in a tectonically active environment and in a sub-tropic climatic zone. However, heavy vegetation covers presents a major problem because the dense vegetation obscures the morphology of underlying landforms. Since 2005, high-resolution airborne LiDAR-DEMs is applied to geological problems such as active fault, deep-seated landslide, surficial mapping and the relationship to earth surface processes. This study demonstrates the efficient use of 1-m-rouslution LiDAR to identify the structure lineament like bedding, fault, cleavage and deep-seated landslide in northeastern Taiwan. Integrated approaches that use grayscale slope images, openness with a tint color slope visualization, the three-dimensional (3D) perspective of a red relief image map, and a field investigation are employed to identify the aforementioned features. In this study, the previously inferred Huanshan Fault is confirmed as a NE-SW-trending, systematic parallel river channel and continuous lineaments in the openness images are interpreted as regional attitude, and a field investigation confirms that interpretation. Signatures of deep-seated landslides are successfully differentiated in LiDAR DEM images and 25-cm-resoultion aerial photography by using different visualization techniques in the upper stream of Lanyang river. Compared with stream drainage system and alluvial terraces distribution between Lanyang and Dajia watershed, is very common in such regions as are characterized by river capture. When a river is extending its channel upstream by headword erosion.
APA, Harvard, Vancouver, ISO, and other styles
8

Wampler, Peter J. "Geology, hydrothermal alteration, and geographic information system analysis of the Zortman Mine area, Montana." Thesis, 1994. http://hdl.handle.net/1957/36221.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Books on the topic "Geological mapping/Maseno area"

1

Chapola, L. S. Geological mapping in the Feremu II area: An appreciation report. Geological Survey Dept., 1989.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
2

Reilly, B. A. Reconnaissance bedrock geological mapping, Misaw Lake area (NTS 64M-NE). Saskatchewan Energy and Mines, Saskatchewan Geological Survey, 1993.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
3

Forum on Geologic Mapping Applications in the Washington-Baltimore Urban Area (1997 Reston, Va.). Forum on Geologic Mapping Applications in the Washington-Baltimore Urban Area: Proceedings, Reston, Virginia, April 23, 1997. U.S. G.P.O., 1997.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Reilly, B. A. Bedrock geological mapping, Hatle Lake area (part of NTS 64M-13 and -14). Saskatchewan Energy and Mines, Saskatchewan Geological Survey, 1993.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Shakides, Emma. Geological mapping and palaeoenvironmental investigations in the Aljariz area, western Vera Basin, S.E. Spain. University of Greenwich, 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Wampler, Peter J. Geology, hydrothermal alteration, and geographic information system analysis of the Zortman Mine area, Montana. 1994.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Geological Survey (U.S.), ed. Status of Shallow-Aquifer Mapping in the Northern Front Range Area, Colorado, U.S. Geological Survey, USGS Fact Sheet 069-00, August 2001. s.n., 2001.

Find full text
APA, Harvard, Vancouver, ISO, and other styles

Book chapters on the topic "Geological mapping/Maseno area"

1

Osipov, Victor. "Large-Scale Thematic Geological Mapping of Moscow Area." In Engineering Geology for Society and Territory - Volume 5. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Hewson, Robert, and Thomas Cudahy. "Issues Affecting Geological Mapping with ASTER Data: A Case Study of the Mt Fitton Area, South Australia." In Land Remote Sensing and Global Environmental Change. Springer New York, 2010. http://dx.doi.org/10.1007/978-1-4419-6749-7_13.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Herz, Norman, and Ervan G. Garrison. "Geomorphology in Archaeology." In Geological Methods for Archaeology. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195090246.003.0005.

Full text
Abstract:
Geomorphology is the study of the evolution of landforms. Analysis of surficial deposits provides much of the evidence for changes in landforms over time. These deposits may be residual materials, formed in place by weathering of underlying formations, or may have been formed elsewhere and then transported by wind, water, or humans to their present site of deposition. They include both sediments and soils, which are commonly confused in the field although each originates by different processes and each yields different kinds of information. Both geomorphology and surficial deposits are the principal subjects of several other publications and will not be covered in great detail here. This book aims to cover in more detail fields that are universally acknowledged to be important for archaeology but are generally ignored in the "geoarchaeology" literature. Those seeking more information on geomorphology and surficial deposits should refer to other publications. The kind and amount of surficial materials change with the changing land surface and climatic conditions and so offer the best evidence regarding the evolution of the landscape. An understanding of these changes on a site will allow a re-creation of the paleoenvironment at the time of occupation and a modeling of the prehistoric land-use patterns. Archaeological exploration in an area is facilitated by first pinpointing desirable habitation sites of the time and then targeting these sites for geophysical prospecting. After a site has been discovered, geophysical and geomorphic-sedimentologic information can help develop excavation strategies. Such information commonly allows a better idea of the distribution and nature of buried artifacts and may explain anomalous surficial redistribution of artifacts, for example, by downslope wash or sediment burial. The first study in a new area proposed for any detailed archaeological work should be geomorphic-surficial geology. It can be carried out in three distinct phases:1. Geomorphic mapping affords meaningful descriptions of the landforms, drainage patterns, surficial deposits, tectonic features, and any active geomorphological processes. 2. The erosional processes that carved the landforms—including soil formation, sediment removal or deposition, and tectonic uplift—are documented.
APA, Harvard, Vancouver, ISO, and other styles
4

Datsenko, Liudmyla, and Serhii Kolomiiets. "GROUNDWATERS OF NIKOLSKOHO REGION (DONBASS): GEOLOGY, STRATIGRAPHY, HYDROGEOLOGY, TOPOGRAPHIC AND GEODESIC WORKS." In State, trends and prospects of land sciences, environment, physics, mathematics and statistics’ development (1st. ed). Primedia eLaunch LLC, 2020. http://dx.doi.org/10.36074/stplsepmad.ed-1.03.

Full text
Abstract:
Arid regions of the south of Ukraine (Donetsk, Zaporizhia, Kherson regions) are facing an acute shortage of drinking and technical water, which consumption increases from year to year. A clear understanding of the shortage not only drinking water but also water for fish breeding, cultural and recreational needs is worrying the world scientific community. Understanding of hydrogeological, hydrogeochemical processes is important for groundwater protection, especially in arid regions of the world. The study area is located within the central part of the Priazovsk highland. Administratively, it belongs to Nikolsk Region (formerly Volodarsky Region) in Donetsk Region. There are four research periods in geological mapping and study of the Eastern and North-Western Priazovia region. The most important researches of the late last century include medium-size deep geological mapping of the North-Western and Eastern Priazovia, generalization of all geological materials of the previous researchers, obtaining data from stratigraphy, magmatism, tectonics and metallogeny, hydrogeology, which allowed to significantly clarify the geological structure of the region. The only possible centralized water supply source on the most part of the territory may be an aquifer of Proterozoic crystalline rocks. In the south-eastern part of the territory can be used Sarmatian sands, sandstones and limestone horizon, for the aquifer of crystalline rocks, the most water-rich is the tectonic disturbance zone with open fracturing.
APA, Harvard, Vancouver, ISO, and other styles
5

Robidoux, Philippe, Julie Roberge, and César Adams. "Spatial Visualization of Geochemical Data: Application to the Chichinautzin Volcanic Field, Mexico." In Volcanoes - Updates in Volcanology [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.93798.

Full text
Abstract:
The presence of spatial magma heterogeneities in volcanic monogenetic fields is a major observation discussed as well synthesized for worldwide volcanic fields. Magma heterogeneities still have not been visualized in the form of detailed spatial analyst tools, which could further help structuring works of geological mapping, volcanic hazard, and geoheritage evaluations. Here we synthetized 32 published datasets with a novel geochemical mapping model inspired by sub-disciplines of geomatic in one of the most documented monogenetic fields on earth: the Chichinautzin Volcanic Field (CVF) in Mexico. The volcanic units from CVF are covering the 2500 km2 area, and its neighbor stratovolcanoes are bordering the limit of most volcanic centers (Popocatepetl, Iztaccihuatl, and Nevado de Toluca). The results illustrate polygons and point map symbols from geochemical markers such as Alkalis vs SiO2, Sr/Y, and Ba/Nb. The geochemical heterogeneity of the CVF monogenetic bodies decreases as it approaches the Popocatepetl-Iztaccihuatl stratovolcanoes. This alignment is not observed in the occidental CVF portion near the flank of Nevado de Toluca, but geochemical anomalies associated to markers of continental crust interaction such as Sr/Y follow elongated patterns that are not strictly following structural lines and faults mapped on surface.
APA, Harvard, Vancouver, ISO, and other styles
6

Selinus, O. "Biogeochemical Monitoring in Medical Geology." In Geology and Health. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195162042.003.0029.

Full text
Abstract:
How can we determine the distribution of metals and other elements in our environment? The Geological Survey of Sweden started an innovative monitoring of metals in a monitoring/mapping program in 1980. Before 1980, traditional inorganic stream sediments were used, a method still employed all over the world, but not really suitable for medical work. A new method is used, whereby metal concentrations are determined in organic material consisting of aquatic mosses and roots of aquatic higher plants. These are barrier-free with respect to trace metal uptake and reflect the metal concentrations in stream water (Brundin 1972, 1988, Kabata-Pendias,1992, Selinus 1989). Aerial parts of many plant species do not generally respond to increasing metal concentrations in the growth medium because of physiological barriers between roots and above-ground parts of plants. These barriers protect them from uptake of toxic levels of metals into the vital reproductive organs. The roots and mosses, however, respond closely to chemical variations in background levels related to different bedrock types in addition to effects of pollution. The biogeochemical samples provide information on the time-related bioavailable metal contents in aquatic plants and in the environment. One great advantage of using biogeochemical samples instead of water samples is also that the biogeochemical samples provide integrated information of the metal contents in the water for a period of some years. Water samples suffer from seasonal and annual variations depending on, for example, precipitation. The mapping program now covers about 65% of the land area of Sweden (40,000 sample sites, one sample every 6 km²), where about 80% of the population of Sweden is living. This means that there is now available an extensive analytical data base for use in environmental and medical research (Freden 1994). One example of the use of biogeochemical monitoring concerns high cadmium contents in Sweden. In noncontaminated, noncultivated soils, Cd concentration is largely governed by the amount of Cd in the parent material (Thornton 1986). If the substrate concentration is higher than in background concentrations, Cd is readily taken up by roots and is distributed throughout the plants.
APA, Harvard, Vancouver, ISO, and other styles
7

Amgaa, Tsolmon, Dieter Mader, Wolf Uwe Reimold, and Christian Koeberl. "Tabun Khara Obo impact crater, Mongolia: Geophysics, geology, petrography, and geochemistry." In Large Meteorite Impacts and Planetary Evolution VI. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2550(04).

Full text
Abstract:
ABSTRACT Tabun Khara Obo is the only currently known impact crater in Mongolia. The crater is centered at 44°07′50″N and 109°39′20″E in southeastern Mongolia. Tabun Khara Obo is a 1.3-km-diameter, simple bowl-shaped structure that is well visible in topography and clearly visible on remote-sensing images. The crater is located on a flat, elevated plateau composed of Carboniferous arc-related volcanic and volcanosedimentary rocks metamorphosed to upper amphibolite to greenschist facies (volcaniclastic sandstones, metagraywacke, quartz-feldspar–mica schist, and other schistose sedimentary rocks). Some geophysical data exist for the Tabun Khara Obo structure. The gravity data correlate well with topography. The −2.5–3 mGal anomaly is similar to that of other, similarly sized impact craters. A weak magnetic low over the crater area may be attributed to impact disruption of the regional trend. The Tabun Khara Obo crater is slightly oval in shape and is elongated perpendicular to the regional lithological and foliation trend in a northeasterly direction. This may be a result of crater modification, when rocks of the crater rim preferentially slumped along fracture planes parallel to the regional structural trend. Radial and tangential faults and fractures occur abundantly along the periphery of the crater. Breccias occur along the crater periphery as well, mostly in the E-NE parts of the structure. Monomict breccias form narrow (&amp;lt;1 m) lenses, and polymict breccias cover the outer flank of the eastern crater rim. While geophysical and morphological data are consistent with expectations for an impact crater, no diagnostic evidence for shock metamorphism, such as planar deformation features or shatter cones, was demonstrated by earlier authors. As it is commonly difficult to find convincing impact evidence at small craters, we carried out further geological and geophysical work in 2005–2007 and drilling in 2007–2008. Surface mapping and sampling did not reveal structural, mineralogical, or geochemical evidence for an impact origin. In 2008, we drilled into the center of the crater to a maximum depth of 206 m, with 135 m of core recovery. From the top, the core consists of 3 m of eolian sand, 137 m of lake deposits (mud, evaporites), 34 m of lake deposits (gypsum with carbonate and mud), 11 m of polymict breccia (with greenschist and gneiss clasts), and 19 m of monomict breccia (brecciated quartz-feldspar–mica schist). The breccias start at 174 m depth as polymict breccias with angular clasts of different lithologies and gradually change downward to breccias constituting the dominant lithology, until finally grading into monomict breccia. At the bottom of the borehole, we noted strongly brecciated quartz-feldspar schist. The breccia cement also changes over this interval from gypsum and carbonate cement to fine-grained clastic matrix. Some quartz grains from breccia samples from 192, 194.2, 196.4, 199.3, 201.6, and 204 m depth showed planar deformation features with impact-characteristic orientations. This discovery of unambiguous shock features in drill core samples confirms the impact origin of the Tabun Khara Obo crater. The age of the structure is not yet known. Currently, it is only poorly constrained to post-Cretaceous on stratigraphic grounds.
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Geological mapping/Maseno area"

1

Yuxin Li, Weiming Li, Min Qing, and Qun Wang. "Applying three-dimensional visualization technology in the area of remote sensing geological mapping." In 2011 International Conference on Multimedia Technology (ICMT). IEEE, 2011. http://dx.doi.org/10.1109/icmt.2011.6002238.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Zheng, Bing, Diquan Diquan Li, and Maojun Tian. "Application of Wide Field Electromagnetic Method in the Geological Mapping of Benxi Ore Concentration Area." In 7th International Conference on Environment and Engineering Geophysics & Summit Forum of Chinese Academy of Engineering on Engineering Science and Technology. Atlantis Press, 2016. http://dx.doi.org/10.2991/iceeg-16.2016.26.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Kurniawan, A. P. "Possible Mesozoic Graben in The Klamono Area Based on New Geological Field Mapping and 3D Seismic Data." In Indonesian Petroleum Association 42nd Annual Convention and Exhibition. Indonesian Petroleum Association, 2018. http://dx.doi.org/10.29118/ipa19.g.138.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Labbassi, Kamal, Amina Tajdi, and Ahmed Er-raji. "Remote sensing and geological mapping for a groundwater recharge model in the arid area of Sebt Rbrykine: Doukkala, western Morocco." In 2009 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2009. http://dx.doi.org/10.1109/igarss.2009.5416898.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Barr, Sandra M., Chris E. White, Deanne van Rooyen, Lisa R. Slaman, and Jonathan M. Shute. "THE CHETICAMP AREA, CAPE BRETON ISLAND, NOVA SCOTIA: A GEOLOGICAL ENIGMA PARTLY RESOLVED BY MAPPING, U-PB (ZIRCON) GEOCHRONOLOGY, AND PETROLOGY." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-271869.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Sadek, Mohamed F., and Safaa M. Hassan. "Rock discrimination and geological mapping of basement rocks at Gabal Gharib area north eastern desert of Egypt with application of landsat ETM and Egyptsat-1 data." In SPIE Europe Remote Sensing, edited by Ulrich Michel and Daniel L. Civco. SPIE, 2009. http://dx.doi.org/10.1117/12.829752.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Clegg, Nigel Mark, Ana Beatriz Domingues, Rosamary Ameneiro Paredes, et al. "Mapping Complex Geological Surface Morphology During Landing Operations Using 3-D Inversion of Ultra-Deep Electromagnetic LWD Data." In Offshore Technology Conference. OTC, 2021. http://dx.doi.org/10.4043/31216-ms.

Full text
Abstract:
Abstract Ultra-deep azimuthal electromagnetic (EM) logging-while-drilling (LWD) tools are frequently used during landing operations for early detection of the reservoir top. This enables alterations to the well plan before the reservoir is penetrated. To date, this approach has relied on one-dimensional (1-D) inversions that accounts only for changes in resistivity above or below the wellbore. When geology is complex, resulting in lateral changes in resistivity, 3-D inversion of EM data is required to provide increased reservoir understanding. This paper presents a case study from offshore Brazil, targeting a turbidite deposit. A complex reservoir surface was expected, as defined by seismic data for the area. Although top structure rugosity and lateral position uncertainty had been incorporated into the prognosis, the impact of surface topography on inversion results while landing was not anticipated. During real-time operations, 1-D EM inversion was used along with correlation of shallow LWD data to map the reservoir top. It was clear the geology was more complicated than depicted by the 2-D geological model constructed from the 1-D inversion and that lateral changes in surface morphology may be occurring. Post well a 3-D inversion of the EM data revealed the 3-D geological structure. During the initial approach, the 1-D inversion indicated that relief of the reservoir top was more exaggerated than expected; the well intersected a sharp peak prior to approaching the target zone. The misfit on the 1-D inversion indicated there was potential for lateral variation in resistivity, influencing the 1-D results; lateral changes can produce artefacts that obscure the subsurface structure. This was confirmed after drilling with analysis of ultra-deep azimuthal resistivity images, indicating significant changes in resistivity to the left and right of the borehole. A 3-D EM inversion was run to depict these complex subsurface geometries. The 1-D inversion results were better understood post-drill with the 3-D inversion results, which show a high point in the reservoir top to the side of the wellbore that was drilled past, but not penetrated by, the well. This high-resistivity zone had a negative effect on the 1-D inversion results and made delineation of the reservoir top difficult. Understanding lateral variations in formation and fluid boundaries can improve well placement and reservoir understanding. This knowledge can impact landing scenarios and well placement within the reservoir. Three-dimensional inversion of ultra-deep azimuthal EM LWD data in real time will provide a clearer picture of the position of resistivity changes while drilling. This will enable decisions to be made that affect the azimuthal position of a well, as well as its vertical position during drilling, thereby facilitating optimal well placement, even in complex geological environments or for infill wells requiring precise well placement.
APA, Harvard, Vancouver, ISO, and other styles
8

Andika, B. "Characteristics of Facies Associations, Ichnofacies and Microfossils for Depositional Environment Interpretation of The Clastic Pulau Balang Formation, Samarinda." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-sg-12.

Full text
Abstract:
The Kutai Basin contains prolific reserves of oil and gas. The study of depositional environments is one of the goals of oil and gas exploration. The location of this research is situated in the Tanah Merah area, Samarinda. The objective of this research was to analyse outcrops of the Pulau Balang Formation exposed in the Tanah Merah area to determine the depositional environment. Site specific studies were conducted at 3 localities in this area; TM1, TM2 and TM3. This study combines geological mapping, measured sections, facies analysis, petrography, ichnofacies analysis and microfossil analysis. Geological mapping was carried out to determine the distribution of rock units and geological structures. Measured sections were used for facies analysis and the identification of sedimentary structures and ichnofacies. Petrography was carried out to determine the mineral content of rocks and microfossil analysis for palaeobathymetric environmental analysis. The geological structure of the study area comprises a NE-SW trending anticline and syncline and a left lateral strike-slip fault with E-W direction. The study area is entirely within the Middle Miocene age Pulau Balang Formation and can be divided into three facies associations. The TM1 facies association comprises strata interpreted to be deposited in a supratidal marsh and intertidal flat environment. The TM2 facies association comprises strata interpreted to be deposited in a subtidal, intertidal, and supratidal environment. The TM3 facies association comprises strata interpreted to be deposited in a shoreface environment. The petrography of the study area indicates that rock units predominantly comprise quartz wacke and lithic wacke. Two ichnofacies were identified in the research area 2, namely the Skolithos ichnofacies and the Skolithos-Cruziana ichnofacies and contain ichnogenera namely Ophiomorpha, Skolithos, Planolites, Thalassinoides, Paaleophycus. Microfossil analysis found benthonic foraminifera species including Nodosaria lamellala, N. radicula, Vaginulinopsis tricarinata, Lagena costata, Striatissima vaginulina, Bulimina lappa, Planularia auris, Quinqueloculina seminulum, Bolivina punctata and Lahena laevis. Based on the presence of these microfossils and ichnofacies, it is interpreted that the research area was deposited in a neritic-bathyal environment.
APA, Harvard, Vancouver, ISO, and other styles
9

Drápela, Emil. "Mapping of urban geoheritage in city of Liberec using participatory research." In 27th edition of the Central European Conference with subtitle (Teaching) of regional geography. Masaryk University Press, 2020. http://dx.doi.org/10.5817/cz.muni.p210-9694-2020-2.

Full text
Abstract:
Urban geoheritage is a phenomenon that is present in almost every city, but so far, only some cities use it as a tourist product. In May and June 2019, in order to create an urban geoheritage trail in Liberec, it was mapped in the wider city centre. Considering the vastness of the area, mapping was carried out by volunteers who were interested in the topic of popularization of geology but did not have the expertise of geological knowledge. This lack of expertise may seem to be a significant limiting factor, but in fact, it is a positive thing, as the knowledge of the mapping volunteer is at a similar (low) level to the future user of the educational trail. Thus, in the evaluation of geosites, the expert-layman barrier is eliminated and the benefit is the feedback of the future user. However, participatory research has its own specifics, which must be adapted to the methodology used. First, it is to ensure the homogeneity of the data that is collected by a large number of volunteers and which can be influenced by subjective influences. Furthermore, it is their professional value and practical application. Finally, yet importantly, the technical parameters of data that will be further processed in GIS. This paper describes the research methodology used and summarizes the experience with the use of participatory research for the purpose of mapping urban geoheritage in Liberec.
APA, Harvard, Vancouver, ISO, and other styles
10

Reka, D. ,. S. "Rembang Zone Petroleum Play, Stratigraphic and Petrographic Analysis of Ngrayong Formation as Reservoir, Jamprong Area, Tuban, East Java." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-sg-326.

Full text
Abstract:
The following research took place in the Jamprong area, Tuban Regency, East Java Province within a study area of 2 km2. Physiographically, the study area is situated in the anticlinorium of the Rembang Zone. This research aims to define the reservoir potential of outcrop samples from the Ngrayong Formation as an analogue for the subsurface. In addition, the depositional environment and the age of the rock in the research area was determined. The Ngrayong Formation is regarded as a potential reservoir in the North East Java Basin. The accumulated data consists of stratigraphy, petrographic analysisand paleontological analysis of rock samples, and geological mapping has been carried out to determine the distribution of rocks. Facies were determined based on outcrop observations and comprise predominantly arkose sandstone facies with fine – coarse grained, moderately sorted and with cross-bedding, herringbone, and lamination, and another facies namely massive carbonate grainstone. Based on these facies, the interpreted depositional environment is the transition of tidal flat to shallow marine carbonate platform with relative biostratigraphic age of Middle Miocene, Langhian to Serravallian (M6-M8 planktonic foraminiferal biozones). Rocks in the study area have porosity &gt;20% or very good and permeability &gt;130 or fair based on petrographic observations, and this supports the interpretation of the Ngrayong Formations as a potential reservoir of hydrocarbons.
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Geological mapping/Maseno area"

1

Dodds, C. J. Geological mapping in Tatshenshini River map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122684.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Haggart, J. W., G. J. Woodsworth, and A. Justason. Update on geological mapping, southeast Nass River map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209489.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Gordey, S. P. Teslin map area, a New Geological Mapping Project in southern Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132511.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Hickson, C. J., P. Read, W. H. Mathews, J. A. Hunt, G. Johansson, and G. E. Rouse. Revised Geological Mapping of northeastern Taseko Lakes map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132515.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

van der Heyden, P., G. J. Woodsworth, and L. D. Snyder. Reconnaissance geological mapping in southwest Nass River map area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211132.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Sharpe, D. R., P. J. Barnett, H. A. J. Russell, T. A. Brennand, and G. Gorrell. Regional geological mapping of the Oak Ridges Moraine, Greater Toronto area, southern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210859.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Ryan, J. J., and S. P. Gordey. New geological mapping in Yukon-Tanana terrane near Thistle Creek, Stewart River map area, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/211986.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Ryan, J. J., S. P. Gordey, P. Glombick, S. J. Piercey, and M E Villeneuve. Update on bedrock geological mapping of the Yukon-Tanana terrane, southern Stewart River map area, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214026.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Rencz, A. N., D. Baril, and P. H. Thompson. Integrating LANDSAT, aeromagnetic, and geological data for regional bedrock mapping, Winter Lake-Lac de Gras map area, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/184117.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Reilly, B. A., D. J. Thomas, W. L. Slimmon, K. E. Ashton, and C T Harper. Project Seagull: a multi-disciplinary approach to revisional geological bedrock mapping along the Precambrian Shield Margin in the Flin Flon-Amisk Lake area. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205402.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Geological mapping/Maseno area' for particular source types:
Journal articles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography