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Journal articles on the topic 'Sedimentary terrain'

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1

Ibrahim, Ibrahim O., Adekunle Rahman Rasaq, Ibrahim Kehinde Olojoku, Ibrahim Bilqees Damilola Habeeb, and Abdulbariu Ibrahim. "Comparative Analysis of Aquifer Properties in Selected Geologic Terrain in Nigeria." PROGRESS: A Journal of Multidisciplinary Studies 5, no. 2 (2024): 12–23. https://doi.org/10.71016/tp/efnbyt89.

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Aim of the Study: Two main geologic terrains of basement complex and sedimentary areas were investigated for underground water production capacity by evaluating the aquifer properties. The assessment was done by evaluating 19 boreholes in the two terrains. TK1-TK10 constituted the boreholes from basement area, while AK1-9 constituted boreholes of sedimentary terrain. Methodology: Pumping rate of the boreholes were crucial to establish the water production capacity from the geologic terrains. Dipper, stopwatch, graduated plastic container, 1 h.p submersible pump, 5.5 KVA generator and field not
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2

Byrne, Paul K., Richard C. Ghail, Martha S. Gilmore, et al. "Venus tesserae feature layered, folded, and eroded rocks." Geology 49, no. 1 (2020): 81–85. http://dx.doi.org/10.1130/g47940.1.

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Abstract Tesserae on Venus are locally the stratigraphically oldest units preserved on the planet. These regions are characterized by pervasive tectonic deformation including normal faults, grabens, thrust faults, and folds. In multiple tesserae, sets of (often highly) curved, parallel linear features are also present. These features strongly resemble terracing in layered volcanic or sedimentary sequences on Earth having arcuate or sinuous outcrop patterns that follow undulating topography. Should this analogy hold for Venus, then these outcrop patterns imply some erosion of the tessera units
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Jiang, Lichun, Huazhe Jiao, Bo Xie, and Han Yang. "Study on Safety Coefficient of Sedimentary Bauxite Strip Pillar under Valley Terrain." International Journal of Environmental Research and Public Health 19, no. 17 (2022): 10991. http://dx.doi.org/10.3390/ijerph191710991.

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The underground sedimentary bauxite ore body in Shanxi province has a shallow burial depth; the valley terrain caused stress concentration on a pillar which affected the pillar’s safety and goaf stability. This paper proposed a pillar safety coefficient calculation method affected by the goaf structural parameters and the valley terrain, which was based on a pillar mechanics analysis under the valley terrain. The results show that the overlying valley terrain will cause stress concentration on the pillar, reducing the adequate bearing capacity and the pillar stability. The increase of the goaf
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4

Young, Roger A., and James E. Lucas. "Exploration beneath volcanics: Snake River plain, Idaho." GEOPHYSICS 53, no. 4 (1988): 444–52. http://dx.doi.org/10.1190/1.1442476.

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Coincident gravity, magnetotelluric (MT), and seismic reflection‐refraction surveys were conducted along a line traversing the boundary between the volcanic‐covered Eastern Snake River plain, Idaho, and the sediment‐covered Western overthrust belt, One‐dimensional MT and seismic refraction analysis away from the immediate boundary between sediments and volcanics successfully maps the depths to units of igneous and sedimentary—or metasedimentary—rock. Substantially different models of the volcanic‐covered terrain and of the sediment‐covered terrain are linked by a gravity anomaly and by an elon
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Koroteev, Viktor A., Viktor M. Necheukhin, Artur A. Krasnobaev, and Elena N. Volchek. "Terrains of the main geodynamical types in the structures of Ural-Timan areal and the Eurasia North-Eastern segment." LITOSFERA, no. 6 (December 28, 2018): 779–96. http://dx.doi.org/10.24930/1681-9004-2018-18-6-779-796.

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Subject of study. Different points of view on the concept of structures of the terrain type and their role in the addition of orogenic belts are considered. Materials and methods. We used our own research and analysis of the latest publications about the Ural-Timan region and the Pacific belt, on the territory of the Northeast segment of Eurasia, as well as currently known isotope radiometric data. It was used also the result of geophysical seismotectonic and paleomagnetic explorations. Results. It has been established that in the composition of the Ural-Timan structural area, along with the P
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Tulakov, Ulugbek, Azizbek Khurramov, Madina Khurramova, et al. "The role of land resources improvement and development." E3S Web of Conferences 587 (2024): 04004. http://dx.doi.org/10.1051/e3sconf/202458704004.

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An area that can be defined as land is referred to as land and land resources. It includes all characteristics of the biosphere that are directly above or below the surface of the earth, such as the near-surface, climate, soil and terrain forms, surface hydrology (including shallow lakes, rivers, marshes, and swamps), the near-surface sedimentary layers and the groundwater and geohydrological reserve that are associated with them, the populations of plants and animals, the pattern of human settlement, and the tangible effects of both past and present human activity, such as terracing, water st
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7

Kim, Jinwook, and Hosung Shin. "Soil Depth Prediction Model Using Terrain Attributes in Gangwon-do, South Korea." Applied Sciences 13, no. 3 (2023): 1453. http://dx.doi.org/10.3390/app13031453.

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Soil depth is a crucial parameter in slope stability analysis in mountainous areas. The drilling survey is the most reliable method for determining soil depth, but it requires a high cost for the vast geographical area. Therefore, this study proposes a soil depth prediction model for mountainous areas that uses Terrain Attributes (TAs) from digital maps. Gangwon-Do, a predominantly mountainous region in South Korea, is selected as the study target area. The study area is classified by parent rock type into igneous rocks, metamorphic rocks, and sedimentary rocks. The correlation with TAs is ana
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8

Sutinen, R., I. Aro, P. Närhi, M. Piekkari, and M. Middleton. "Maskevarri Ráhppát in Finnmark, North Norway – is it an earthquake induced landform complex?" Solid Earth Discussions 6, no. 1 (2014): 321–38. http://dx.doi.org/10.5194/sed-6-321-2014.

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Abstract. The Sami word ráhppát means rough bouldery/stony terrain with sharp-relief topography in Finnmark, North Norway. Ráhppáts are common features in the region of the Younger Dryas landforms, yet their origin has remained obscure. The timing of the Younger Dryas is concomitant with the maximum neotectonic fault instability in Fennoscandia, hence earthquake activity was one of the contributing factors for the Younger Dryas morphologies. Ráhppát on the Maskevarri fell, classified as a part of Tromsø-Lyngen sub-stage of the Younger Dryas, was studied by means of geomorphology and measuremen
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9

Hall, Adrian M., Hannah Mathers, and Maarten Krabbendam. "Glacial Ripping in Sedimentary Rocks: Loch Eriboll, NW Scotland." Geosciences 11, no. 6 (2021): 232. http://dx.doi.org/10.3390/geosciences11060232.

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Glacial ripping is a newly recognized process sequence in which subglacial erosion is triggered by groundwater overpressure. Investigations in gneiss terrain in lowland Sweden indicate that ripping involves three stages of (i) hydraulic jacking, (ii) rock disruption under subglacial traction, and (iii) glacial transport of rock blocks. Evidence for each stage includes, respectively, dilated fractures with sediment fills, disintegrated roches moutonnées, and boulder spreads. Here, we ask: can glacial ripping also occur in sedimentary rocks, and, if so, what are its effects? The case study area
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10

Hofmann, A., PH GM Dirks, and H. A. Jelsma. "Late Archaean clastic sedimentary rocks (Shamvaian Group) of the Zimbabwe craton: first observations from the Bindura-Shamva greenstone belt." Canadian Journal of Earth Sciences 39, no. 11 (2002): 1689–708. http://dx.doi.org/10.1139/e02-074.

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The ~2.65 Ga old Shamvaian Group sedimentary rocks occur as a folded succession in the central part of the Bindura–Shamva greenstone belt of Zimbabwe. The strata comprise distinct, shear zone-bounded tectonostratigraphic units which may be stratigraphically arranged as follows. The lower part of the succession is represented by a transgressive, fining-upward sequence of alluvial fan conglomerate, overlain by fluvial braid-plain pebbly sandstone and marine shoreface sandstone. Detritus was derived from a mid-Archaean granitoid-gneiss terrain situated to the east. Sediment supply and subsidence
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11

Pan, Xuemei. "Preliminary analysis of sedimentary characteristics and facies model of M-II layer in Kazakhstan Oilfield A." E3S Web of Conferences 352 (2022): 01041. http://dx.doi.org/10.1051/e3sconf/202235201041.

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The lithologic melange accumulation of areskum formation in akshabluk area is one of the key strata in exploration. Its basement inheritance controls the whole process of Jurassic sedimentation, and the filling and leveling gradually reduces the terrain elevation difference; After the late Jurassic deformation, the flat paleogeomorphology was changed and the deposition of Early Cretaceous strata was controlled. Under the control of marker beds, sedimentary cycles are divided according to the cycle characteristics of logging curves. Under the control of cycle interface (standard layer), accordi
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Ariyo, S.O, and A.A Banjo. "APPLICATION OF ELECTRICAL RESISTIVITY METHOD FOR GROUNDWATER EXPLORATION IN A SEDIMENTARY TERRAIN. A CASE STUDY OF ILARA-REMO, SOUTHWESTERN NIGERIA." Continental J. Earth Sciences 3 (July 7, 2008): 53–58. https://doi.org/10.5281/zenodo.824306.

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A geophysical evaluation using Electrical Resistivity method for groundwater exploration at Ilara-Remo, southwestern Nigeria was carried out. The investigation involved the utilization of Vertical Electrical Sounding (VES) technique with schlumberger electrode array system. The studied area is located within the sedimentary basin (Dahomey basin) of southwestern Nigeria, ferrigenous sandstone was found to be the major rock type in the study area. The data acquired from the ten (10) VES stations were interpreted using the partial curve matching method and computer assisted iteration technique. T
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13

CORRÊA, IRAN CARLOS STALLIVIERE, RICARDO NORBERTO AYUP ZOUAIN, JAIR WESCHENFELDER, and LUIZ JOSÉ TOMAZELLI. "Áreas Fontes dos Minerais Pesados e sua Distribuição sobre a Plataforma Continental Sul-brasileira, Uruguaia e Norte-argentina." Pesquisas em Geociências 35, no. 1 (2008): 137. http://dx.doi.org/10.22456/1807-9806.17899.

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The heavy mineral fraction of sedimentary rocks and sediments can provide important information about provenance in sedimentary basins studies because some minerals or group of minerals can be traced to a source rock or terrain of specific composition. This work is a provenance study based on heavy mineral analyses of samples collected on the Rio Grande do Sul (southern Brazil), Uruguay and north of Argentine continental shelf (between 29º30´ and 37º 30´ south latitude and 48º 30´ and 56º 30´ west longitude). The fine and very fine sand fractions (2-4 Φ) were selected for heavy mineral analysi
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14

Shandini, Yves, Patrice Arnaud Kouske, Severin Nguiya, and Mouzong Pemi Marcelin. "Structural setting of the Koum sedimentary basin (north Cameroon) derived from EGM2008 gravity field interpretation." Contributions to Geophysics and Geodesy 48, no. 4 (2018): 281–98. http://dx.doi.org/10.2478/congeo-2018-0013.

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Abstract This study is a contribution to the planning of hydrocarbon exploration program of the Koum sedimentary basin in North Cameroon. 3D modeling of WGM2012 gravity data derived from EGM2008 geopotential model in the Koum basin was used together with existing geological and spectral analysis information to give structural picture of the basin. The 3D model of the Koum basin confirms that the basin is developed as a half graben bounded by sub-vertical faults. The thickness of the Cenozoic sediments is about 1.5 km in the eastern part and reaches 4.5 km in the western part of the basin. Grav
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15

Hermawan, Oktanius Richard, and Doni Prakasa Eka Putra. "The Effectiveness of Wenner-Schlumberger and Dipole-dipole Array of 2D Geoelectrical Survey to Detect The Occurring of Groundwater in the Gunung Kidul Karst Aquifer System, Yogyakarta, Indonesia." Journal of Applied Geology 1, no. 2 (2016): 71. http://dx.doi.org/10.22146/jag.26963.

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Until today, geoelectrical survey is the most effective method for groundwater exploration. 2D method or known as horizontal profiling is now the most appropriate method in the geoelectrical survey compare to vertical electrical sounding method. The 2D method of Wenner-Schlumberger and Dipole-dipole configuration proved to be very effective to locate conventional aquifer occurrence on volcanic terrain or sedimentary terrain. Karst aquifer system is an unconventional aquifer and acts very differ in contrast with the conventional sedimentary aquifer. Heterogeneity and discontinuity of limestones
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16

Almeida-Filho, Raimundo, Dilce F. Rossetti, Fernando P. Miranda, Francisco J. Ferreira, Clauzionor Silva, and Carlos Beisl. "Quaternary reactivation of a basement structure in the Barreirinhas Basin, Brazilian Equatorial Margin." Quaternary Research 72, no. 1 (2009): 103–10. http://dx.doi.org/10.1016/j.yqres.2009.02.010.

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AbstractThe Pirapemas Lineament is a remarkable 200-km-long, NE–SW trending structure in the Barreirinhas Basin, one of the several Brazilian coastal basins. This lineament splits the study area in two sectors of distinctive morphology, drainage patterns, and sedimentary covers. Terrain northward of the lineament presents a smooth topography with sub-parallel to sub-dendritic drainage patterns, whereas a dissected plateau characterized by incised valleys and rectangular drainage pattern occurs southward, suggesting a structural control by joints and faults. Geological field data, crossed with
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17

Adegoke Ige, Aladeboyeje, Coker Joseph Olakunle, Agbasi Okechukwu Ebuka, and Inyang Namdie Joseph. "Hydrogeological appraisal of basement and sedimentary terrain in Ogun state using Geoelectrical methods." International Journal of Advanced Geosciences 8, no. 1 (2020): 95. http://dx.doi.org/10.14419/ijag.v8i1.30848.

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The coverage of the groundwater potential was estimated using the geometry calculator, the potential groundwater zones were validated using geophysical surveyed points of some selected locations in Abeokuta and Ewekoro. Generally, the result of the study shows that the higher the aquifer thickness and depth the better the groundwater potential. In the basement part of the study area (Abeokuta), the Northwestern region is characterized by increase in overburden thickness (28.1 m at VES-9), weathered layer resistivity (546 Ω m at VES-7) and longitudinal conductance unit (0.193 S at VES-3 and 0.2
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18

Oteng Mensah, Felix, Clement Alo, and Sandow Mark Yidana. "Evaluation of Groundwater Recharge Estimates in a Partially Metamorphosed Sedimentary Basin in a Tropical Environment: Application of Natural Tracers." Scientific World Journal 2014 (2014): 1–8. http://dx.doi.org/10.1155/2014/419508.

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This study tests the representativeness of groundwater recharge estimates through the chloride mass balance (CMB) method in a tropical environment. The representativeness of recharge estimates using this methodology is tested using evaporation estimates from isotope data, the general spatial distribution of the potential field, and the topographical variations in the area. This study suggests that annual groundwater recharge rates in the area ranges between 0.9% and 21% of annual precipitation. These estimates are consistent with evaporation rates computed from stable isotope data of groundwat
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Cui, Liwei, Nan Peng, Yongqing Liu, Dawei Qiao, and Yanxue Liu. "Sedimentary Filling Evolution under Paleoclimate Transition—A Case Study from the Middle Jurassic Zhiluo Formation, Ordos Basin." Minerals 13, no. 3 (2023): 314. http://dx.doi.org/10.3390/min13030314.

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Under a specific tectonic background, the change in paleoclimate can show different facies associations and depositional architecture. The Jurassic China continent was an important region for transforming the Paleotethys tectonic domain to the circum-Pacific tectonic domain, and its paleoclimate information was entirely preserved in the continental sedimentary successions. The Middle Jurassic Zhiluo Formation, in the Ordos Basin, was at just the critical period of paleostructure and paleoclimate transition, preserving considerable sedimentological evidence; however, little sedimentological res
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Nsikak E., Bassey, and George Nyakno J. "GEOLOGICAL INTERPRETATION OF LANDSAT IMAGERY OF NIGERIA’S HAWAL PRECAMBRIAN BASEMENT COMPLEX TERRAIN." Geological Behavior 7, no. 1 (2023): 16–21. http://dx.doi.org/10.26480/gbr.01.2023.16.21.

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The Hawal Basement Complex is located in Nigeria’s NE region. Satellite imagery used in this study covers longitude 12º 00’ to 13º 30’E, and latitudes 9º 30’ to 11º 00’N. The aim of the study is to decipher the regional geologic structures based on analysis and to determine the mineralization implications from the landsat lineament data. The total land surface area covered is about 23,674.88 km2 and includes part of the north sector of Yola sedimentary Rift Basin. The data consists of LANDSAT TM and SPOT XS scenes collated as mosaics. The imagery was monoscopically studied. Classical aerial im
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Bose, Utpal, and A. K. Sharma. "The Volcano-Sedimentary Association of the Precambrian Hindoli Supracrustals in Southeast Rajasthan." Journal Geological Society of India 40, no. 4 (1992): 359–69. http://dx.doi.org/10.17491/jgsi/1992/400405.

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Abstract An arcuate belt of Precambrian vo1cano-sedimentaries, designated as the Hindoli Group, is sandwiched between the cratonic Archaean Banded Gneissic Complex terrain and the platformal Vindhyan sediments. Turbidites of mainly quartz wacke and petites with interlayered lava flows and tuffs of basalt, basaltic andesite and daciterhyodacite composition constitute the bulk of the Hindoli vo1cano~sedimentaries. These are interpreted to have been deposited in a continent-marginal basin with active participation of an arc system. Toward the end of the basin evolutioo; the continent-margin acted
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Constable, Steven, Kerry Key, and Lisl Lewis. "Mapping offshore sedimentary structure using electromagnetic methods and terrain effects in marine magnetotelluric data." Geophysical Journal International 176, no. 2 (2009): 431–42. http://dx.doi.org/10.1111/j.1365-246x.2008.03975.x.

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Nguyen, Van Diep, Quoc Hung Duong, Duc Dong Mai, Viet Dung Bui, and Quang Dung Nguyen. "Modern sediment characteristics of Cua Dat hydroelectric reservoir based on high-resolution seismic data." Vietnam Journal of Marine Science and Technology 24, no. 1 (2024): 47–57. http://dx.doi.org/10.15625/1859-3097/20177.

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The high-resolution seismic survey work was conducted in the reservoir area of the Cua Dat hydroelectric using the Sub-bottom Profiler EdgeTech 3400 equipment combination, covering a survey route of over 40 km. The collected data revealed the reservoir area's fundamental terrain and modern sediment characteristics. These findings provided insights into the dynamics of the sedimentary environment on the reservoir surface, indicating that the reservoir's current operational and exploitation conditions can ensure longevity and safety according to the design of the Cua Dat hydroelectric project.
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Huang, Yuhang, Xinghe Yu, and Chao Fu. "Depositional Architecture of Aggrading Delta Front Distributary Channels and Corresponding Depositional Evolution Process in Ordos Basin: Implications for Deltaic Reservoir Prediction." Water 17, no. 4 (2025): 528. https://doi.org/10.3390/w17040528.

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Distributary channels at the delta front of lacustrine basins play a crucial role in transporting terrigenous sediments and redistributing depositional facies along the basin margin. These channels are also significant reservoirs for oil and gas. This study investigates the Triassic Yanchang Formation in the Southeastern Ordos Basin (China), emphasizing the sedimentary characteristics, hydrodynamic processes, and evolutionary patterns of delta front distributary channels. Special focus is given to the response of sedimentary filling to paleotopographic changes along the basin margin to enhance
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Birgisson, Bjorn, and Byron E. Ruth. "Improving Performance Through Consideration of Terrain Conditions: Soils, Drainage, and Climate." Transportation Research Record: Journal of the Transportation Research Board 1819, no. 1 (2003): 369–77. http://dx.doi.org/10.3141/1819b-47.

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Inadequate drainage of surface and subsurface water can have significant impact on pavement behavior and long-term maintenance costs. Interception of water before it infiltrates into the pavement foundation is essential unless the soils are truly free draining. Even then, there can be potential damage by frost action. Identification of seepage zones and surface runoff characteristics based on terrain conditions such as soils and geology can aid in the selection of a suitable road alignment and design to minimize future problems. However, most moisture–soil-related pavement performance problems
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26

Vasudev, V. N., and Ananda Deb Mukherjee. "Sulphide are Mineralisation in Archaean Volcanogene-Sedimentary Ensemble of Ganacharpura, Kolar Greenstone Belt, Dharwar Craton, India." Journal Geological Society of India 27, no. 3 (1986): 274–81. http://dx.doi.org/10.17491/jgsi/1986/270304.

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Abstract Stratiform pyrrhotitic sulphide ores occur at Ganacharpura which forms a part of mafic volcanic and volcano-sedimentary terrain of the Archaean Kolar greenstone belt. The ores are interbanded with graphite-quartz-sericite schist and are metamorphosed and deformed along with the associated rock types of the area. Dominant ore mineral is pyrrhotite while chalcopyrite, pyrite, sphalerite, galena, magnetite and mackinawite are present in subordinate amounts. The mineral chemistry of the co-existing sulphide phases indicate equilibration at 587°C and 4.98 Kbar total pressure. The fugacitie
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27

Sutinen, R., I. Aro, P. Närhi, M. Piekkari, and M. Middleton. "Maskevarri Ráhppát in Finnmark, northern Norway – is it an earthquake-induced landform complex?" Solid Earth 5, no. 2 (2014): 683–91. http://dx.doi.org/10.5194/se-5-683-2014.

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Abstract. The Sami word ráhppát means rough bouldery/stony terrain with sharp-relief topography in Finnmark, northern Norway. Ráhppát is a common name in the region of the Younger Dryas landforms, yet the origin of ráhppát has remained obscure. The timing of the Younger Dryas is concomitant with the maximum neotectonic fault instability in Fennoscandia. Hence, earthquake activity may have been one of the contributing factors for the Younger Dryas morphologies. Ráhppát on the Maskevarri fell, classified as a part of Tromsø-Lyngen sub-stage of the Younger Dryas, was studied by means of geomorpho
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28

Aina, Oni Olubukola, Ahzegbobor P. Aizebeokhai, and Boyo Henry Oritsemamididasan. "Analysis of aeromagnetic filtering techniques in locating the primary target in sedimentary terrain: A review." Open Physics 19, no. 1 (2021): 912–20. http://dx.doi.org/10.1515/phys-2021-0045.

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Abstract This article analyzes some aeromagnetic filtering techniques for mitigating deceptive geophysical conceptions that may result in a distorted range of geological information from aeromagnetic data. The implication of using the aeromagnetic method, data processing, and enhancement to distinguish sediment-produced anomalies was considered. Two methods to locate buried faults in aeromagnetic data were compared: Edge and fault detection were considered using the magnetic contrast and horizontal gradient methods, whereas rapid depth estimation was considered using the Euler deconvolution me
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Oyedele, K., and K. Ekpoette. "Resistivity attributes of foundation beds in a sedimentary terrain: Implications on geo-engineering soil conditions." American Journal of Scientific and Industrial Research 2, no. 5 (2011): 734–39. http://dx.doi.org/10.5251/ajsir.2011.2.5.734.739.

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Yeh, Chih-Hsiang, Ming-Lang Lin, Yu-Chang Chan, Kuo-Jen Chang, and Yu-Chung Hsieh. "Dip-slope mapping of sedimentary terrain using polygon auto-tracing and airborne LiDAR topographic data." Engineering Geology 222 (May 2017): 236–49. http://dx.doi.org/10.1016/j.enggeo.2017.04.009.

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Qu, Guohui, Xuebin Tian, Bowen Li, et al. "New Progress in the Study of Siliceous Rock Oil and Gas in Nadanha Single Terrain." E3S Web of Conferences 358 (2022): 02037. http://dx.doi.org/10.1051/e3sconf/202235802037.

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The siliceous shale oil and gas in Nadanhada terrane has been studied through field geological survey, geochemistry and sedimentary petrology. The results show that the area belongs to a good shale reservoir, and the siliceous rock is brittle and suitable for exploitation. The abundance of organic matter is relatively high. From west to east and from south to north, the abundance of organic matter increases and the maturity of organic matter decreases. From west to east and from south to north, the dynamic metamorphism and thermal contact metamorphism of the siliceous rocks in the Nadanhada te
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Kivior, I., and D. Boyd. "THE INTERPRETATION OF AEROMAGNETIC SURVEYS FOR HYDROCARBON EXPLORATION." APPEA Journal 39, no. 1 (1999): 494. http://dx.doi.org/10.1071/aj98030.

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Aeromagnetic surveys have been generally regarded in petroleum exploration as a reconnaissance tool for major structures. They were used commonly in the early stages of exploration to delineate the shape and depth of the sedimentary basin by detecting the strong magnetic contrast between the sediments and the underlying metamorphic basement. Recent developments in the application of computer technology to the study of the earth's magnetic field have significantly extended the scope of aeromagnetic surveys as a tool in the exploration for hydrocarbons. In this paper the two principal methods us
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Ahmed, Farooq, Aimal Khan Kasi, M. Mohibullah, and Razzaq Abdul Manan. "PETROLOGY AND GEOCHEMISTRY OF THE LATE CRETACEOUS PAB FORMATION, WESTERN SULAIMAN FOLD- THRUST- BELT, PAKISTAN: IMPLICATIONS FOR PROVENANCE AND PALEO-WEATHERING." Journal of Mountain Area Research 6 (December 25, 2021): 45. http://dx.doi.org/10.53874/jmar.v6i0.98.

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Late Cretaceous sandstone succession of the Pab Formation in western Sulaiman Fold Thrust belt Pakistan was investigated for petrology and bulk rock chemistry to determine its source terrain, paleo-weathering and tectonic setting. The formation is mainly comprised of sandstone with reddish to maroon color shale and arenaceous limestone. Texturally, the sandstone is fine to coarse grained, sub-angular to well-rounded and moderately to well sorted. The sandstone is petrologically and geochemically classified as quartz arenite to sub lithic arenite. The detritus was mainly derived from plutonic a
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Durn, Goran. "Terra Rossa in the Mediterranean Region: Parent Materials, Composition and Origin." Geologia Croatica 56, no. 1 (2003): 83–100. http://dx.doi.org/10.4154/gc.2003.06.

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In the past, the term “terra rossa” became quite a common indication for all limestone derived red soils in the Mediterranean region. Today, in some classification systems based on the Mediterranean climate as the major soil differentiating criterion, the term terra rossa is used as a name for the soil subclass “Modal Fersiallitic Red soil” when situated on limestones (DUCHAUFOUR, 1982). However, several national soil classifications (e.g. Croatian, Italian, Israeli) retained the term “terra rossa” for the hard limestone derived red soils. The nature and relationship of terra rossa to underlyi
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Prieto, Maria I., Lorena Moscardelli, and Lesli Wood. "Deepwater sedimentary bedforms in a mobile substrate terrain: Examples from the central Gulf of Mexico Basin." Interpretation 9, no. 2 (2021): SB33—SB48. http://dx.doi.org/10.1190/int-2020-0128.1.

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We have used high-resolution geophysical data to investigate depositional and erosional bedforms in two geomorphologic provinces of the deepwater central Gulf of Mexico Basin: (1) the Mad Dog and Atlantis areas in the Sigsbee Escarpment region and (2) the Holstein minibasin within the salt canopy in the slope. Multibeam bathymetry indicates that the seafloor relief in the study areas is highly irregular because it is influenced by the dynamic behavior of underlying salt bodies resulting in the development of diverse bathymetric features. Side-scan images reveal erosional furrows of different m
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Roostaee, Fatemeh, Gholamreza Mortezanejad, Habib Rahimi, and Ali Gholami. "Crustal and uppermost mantle shear-wave velocity structure beneath the Northeastern Iranian Plateau using an analysis of receiver function and surface‑wave tomography." Annals of Geophysics 67, no. 6 (2024): S659. https://doi.org/10.4401/ag-9095.

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In this study, we investigate the crustal velocity structure and Moho discontinuity depth beneath the NE Iran continental collision zone through joint inversion of P receiver function and Rayleigh wave group velocity dispersion curves. Local Rayleigh wave group velocity dispersion curves were estimated using time-frequency analysis method and two-dimensional surface wave tomography method. Our results distinctly highlight prominent changes in velocity structure along both the northern and southern flanks of Daruneh fault, occurring at both the crustal and lithospheric scales. This fault bounda
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Schwamborn, Georg, Hanno Meyer, Grigory Fedorov, Lutz Schirrmeister, and Hans-W. Hubberten. "Ground ice and slope sediments archiving late Quaternary paleoenvironment and paleoclimate signals at the margins of El'gygytgyn Impact Crater, NE Siberia." Quaternary Research 66, no. 2 (2006): 259–72. http://dx.doi.org/10.1016/j.yqres.2006.06.007.

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AbstractAn accumulation terrace close to the El'gygytgyn Impact Crater in northeastern Siberia contains stratigraphic and periglacial evidence of the paleoenvironmental and paleoclimatic history and permafrost dynamics during late Quaternary time. A succession of paleo active-layer deposits that mirror environmental changes records periods favorable for the establishment and growth of ice-wedge polygonal networks and sediment variations. These two elements of the periglacial landscape serve as complementary paleoenvironmental archives that can be traced back to ∼ 14,000 cal yr BP. The slope se
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Jones, Stacie, Kurt Kyser, Matthew Leybourne, Robin Mackie, Adrian Fleming, and Daniel Layton-Matthews. "Paragenesis of gold mineralization at the Kiyuk Lake Project, Kivalliq Region, Nunavut, Canada." Canadian Mineralogist 59, no. 5 (2021): 1133–65. http://dx.doi.org/10.3749/canmin.2000058.

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ABSTRACT Exploration for gold in Nunavut has been primarily focused on Archean greenstone belts in the north and coastal regions of the territory, resulting in large areas of underexplored terrain in the south. The Kiyuk Lake property is located in the underexplored southwest corner of the Kivalliq Region of Nunavut within the Hearne domain of the ∼1.9 Ga western Churchill Province. The property is hosted by Proterozoic calc-silicate and clastic sedimentary units of the Hurwitz Group (<2.4–1.9 Ga) and the unconformably overlying Kiyuk Group (1.9–1.83 Ga). Gold mineralization in Proteroz
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Fajana, Akindeji, Damilare Moses Jolayemi, Akinola Bolaji Eluwole, and Tokunbo Sanmi Fagbemigun. "Hydrocarbon Potential Evaluation of Chad Basin, Northeastern Nigeria Using High-Resolution Aeromagnetic Data." ABUAD International Journal of Natural and Applied Sciences 4, no. 2 (2024): 62–71. https://doi.org/10.53982/aijnas.2024.0402.08-j.

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A cost-effective and non-intrusive aeromagnetic geophysical technique was utilized to reduce exploration uncertainty in the Chad Basin, which is believed to have significant hydrocarbon potential despite limited exploration due to its remote and challenging terrain. By analyzing various derivatives and magnetic attributes extracted from filtered and enhanced aeromagnetic data, the study aimed to highlight potential areas for hydrocarbon generation and preservation, allowing for more focused and detailed geophysical exploration efforts. This study produced several key maps, including a total ma
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Sivtsev, A. I., D. M. Petrov, and Z. E. Ivanova. "Prospects of Oil and Gas Potential of the Middle Paleozonic Deposits of Eastern Yakutia from Historical Viewpoint of Geological Development." IOP Conference Series: Earth and Environmental Science 988, no. 4 (2022): 042031. http://dx.doi.org/10.1088/1755-1315/988/4/042031.

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Abstract The article considers the prospects of oil and gas potential of the Middle Paleozoic deposits of Eastern Yakutia. Based on the study of the peculiarities of bitumen content intervals of the Silurian-Devonian deposits of Selennyakhsky block, it was concluded about high oil and gas potential of the domanicoid Middle Paleozoic deposits of the Omulevsky terrain. Under favorable structural and tectonic conditions and immersion to shallow depths, Middle Paleozoic deposits can contain oil and gas deposits to clarify the most promising subsoil areas, the author’s version of the geological dev
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Bolarinwa, Anthony Temidayo. "Seasonal Variations of Groundwater Chemistry in the Basement and Sedimentary Rocks of Ibadan and Lagos Areas, Southwestern Nigeria." Earth Science Research 7, no. 1 (2017): 55. http://dx.doi.org/10.5539/esr.v7n1p55.

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Hydrochemical investigation of forty boreholes drilled on the basement and sedimentary rocks in Ibadan and Lagos metropolis southwestern Nigeria respectively were carried out in order to determine the portability of the groundwater in both areas and to highlight differences in their chemical characters and variations with seasons. Data obtained indicated that the groundwater in Ibadan area is mainly the Na + Ca – HCO­­3type, while that of Lagos is Na + Ca – C1 + SO4 type. The groundwater chemistry reflects weathering of sodic plagioclase feldspars in the basement rocks as well as arkosic sands
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Miller, Richard D., and Don W. Steeples. "A shallow seismic reflection survey in basalts of the Snake River Plain, Idaho." GEOPHYSICS 55, no. 6 (1990): 761–68. http://dx.doi.org/10.1190/1.1442888.

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The objective of this feasibility study was to determine if the seismic reflection method could help to optimize placement of water‐quality monitoring wells near a radioactive storage facility. Seismic reflections from depths less than 30 m were recorded along a 500 m long line over a basalt, rhyolite, and sedimentary sequence in the Snake River Plain. Some shallow reflections at 40 to 50 ms on the field files are of exceptional quality with frequency exceeding 150 Hz. Reflections and refractions from selected seismograms along the line possess vastly different normal‐moveout (NMO) and apparen
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Vu, Doan Thai, and Van Nam Thai. "The solutions for construction of sea dike and sea embankments system as the sandy mud trap to support mangrove plants in the coastal zone of Hai Phong city, Vietnam." Tạp chí Khoa học và Công nghệ Biển 21, no. 3 (2021): 341–52. http://dx.doi.org/10.15625/1859-3097/16031.

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Mangrove plants play a viral role in protecting the coast, retraining erosion. Especially in areas considered the variable wave conditions, complex dynamic conditions such as the coastal region of Hai Phong city. However, due to various reasons, the development/additional planting of mangrove forests in the coastal area of Hai Phong in some locations has not achieved the desired result. This study was conducted survey measurements of mangroves, terrain, and practical experience to assess the ecological impact of certain dynamic and sedimentary conditions on mangroves. Thereby proposing several
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Yeh, Chih-Hsiang, Yu-Chang Chan, Kuo-Jen Chang, Ming-Lang Lin, and Yu-Chung Hsieh. "Derivation of Strike and Dip in Sedimentary Terrain Using 3D Image Interpretation Based on Airborne LiDAR Data." Terrestrial, Atmospheric and Oceanic Sciences 25, no. 6 (2014): 775. http://dx.doi.org/10.3319/tao.2014.07.02.01(tt).

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Fasunwon, O. O., A. O. Ayeni, and A. O. Lawal. "A Comparative Study of Borehole Water Quality from Sedimentary Terrain and Basement Complex in South-Western, Nigeria." Research Journal of Environmental Sciences 4, no. 3 (2010): 327–35. http://dx.doi.org/10.3923/rjes.2010.327.335.

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Aizebeokhai, Ahzegbobor P., and Kehinde D. Oyeyemi. "Application of geoelectrical resistivity imaging and VLF-EM for subsurface characterization in a sedimentary terrain, Southwestern Nigeria." Arabian Journal of Geosciences 8, no. 6 (2014): 4083–99. http://dx.doi.org/10.1007/s12517-014-1482-z.

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47

Feinstein, S., G. K. Williams, L. R. Snowdon, F. Goodarzi, and T. Gentzis. "Thermal maturation of organic matter in the Middle Devonian to Tertiary section, Fort Norman area (central Mackenzie Plain)." Canadian Journal of Earth Sciences 28, no. 7 (1991): 1009–18. http://dx.doi.org/10.1139/e91-092.

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The Fort Norman area is marked by a complex structural and depositional history with temporally and spatially variable temperature and maturity gradients. Maturity of the Middle Devonian Canol – Hare Indian unit indicates two terrains of markedly different paleotemperatures and thermal gradients, roughly coinciding with the Palaeozoic Keele Arch (north) and Root Basin (south), with a sharp transition (lateral discontinuity) between them. Maturity of the unconformably overlying Cretaceous to early tertiary section is lower and laterally continuous across the entire study area, showing no relati
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Adeola, Adewole John, Adeyemi Moyosoluwa Odunayo, and Omojola Damilola Ifeoluwa. "Geochemical and mineralogical characteristics of clay deposits at Ijesha–Ijebu and its environs, southwestern Nigeria." Global Journal of Pure and Applied Sciences 26, no. 2 (2020): 119–30. http://dx.doi.org/10.4314/gjpas.v26i2.4.

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Two residual clay deposits and one transported clay deposit in Ijesha-Ijebu area were investigated for their mineralogical, chemical and industrial properties. The investigation was to evaluate their industrial applications and economic importance. The mineralogy of the clay samples was determined using X-ray Diffraction (XRD). The chemical composition of the clay samples was determined using Inductively Coupled Plasma-Mass Spectrometer (ICP-MS). Physical tests which include; thermal properties, plasticity tests, density measurement, linear shrinkage and water absorption capacity were determin
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Liu, Shih-Hung, Robert Hebenstreit, and Margot Böse. "Late Quaternary landform evolution and sedimentary successions in the Miaoli Tableland, northwestern Taiwan." E&G Quaternary Science Journal 71, no. 1 (2022): 1–22. http://dx.doi.org/10.5194/egqsj-71-1-2022.

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Abstract. Elevated Quaternary sedimentary complexes in the western foreland of the central mountain ranges of Taiwan are called tablelands. Their mostly flat surfaces are deeply incised by fluvial processes. The landforms and the fluvial systems in the Miaoli Tableland are investigated by high-resolution terrain analyses based on different datasets. Sediments are described in 51 outcrops and characterized by grain size composition. The outcrops revealed complete or incomplete sequences of the general scheme from bottom to top: sandy tidal–coastal units overlain by gravel- and cobble-rich fluvi
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Shvarev, S. V. "Postglacial seismogenic deformations of an esker in the Northern Karelian Isthmus (south-east Fennoscandia)." Geomorphology RAS, no. 3 (September 11, 2019): 19–35. http://dx.doi.org/10.31857/s0435-42812019319-35.

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The research area is located in the Northern part of the Karelian Isthmus between Lake Ladoga and the Gulf of Finland of the Baltic Sea. The terrain features are closely related to the tectonic structure of the crystalline basement, partially covered with thin deposition layer of the Last Glaciation and Holocene mostly. Accumulative forms are rarely but strongly correlated with the tectonic structure also. Most expressive features of accumulative topography are esker ridges that stretch for tens of kilometers. Analysis of eskers spatial distribution shows their close connection with the struct
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