Relevant bibliographies by topics / Department of Geology and Geophysics

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

Academic literature on the topic 'Department of Geology and Geophysics'

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

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Journal articles on the topic "Department of Geology and Geophysics"

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Jackowski, Antoni, and Kazimierz Krzemień. "Maurycy Pius Rudzki and the birth of geophysics." History of Geo- and Space Sciences 7, no. 1 (February 25, 2016): 23–25. http://dx.doi.org/10.5194/hgss-7-23-2016.

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Abstract. The article describes briefly the life and fundamental work of Rudzki in geology, geography, seismology, oceanography and meteorology. In 1895 he became head of the world's first department of geophysics and meteorology at the Jagiellonian University of Kraków, the second oldest university north of the Alps (Prague being the oldest).
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Carlton, D. P. "The Geophysics Department of Humble Oil and Refining Company (1924–1945)." Leading Edge 23, no. 2 (February 2004): 123–27. http://dx.doi.org/10.1190/1.1651456.

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Khodijah, Siti, Candra Kusuma, and Henny Purnamasari. "OPTIMALISASI PENGEBORAN STERILISASI DAN VERIFIKASI HASIL 3D IP SURVEI DI PARBOTIKAN, MARTABE GOLD MINE, SUMATERA UTARA." Prosiding Temu Profesi Tahunan PERHAPI 1, no. 1 (March 29, 2020): 263–74. http://dx.doi.org/10.36986/ptptp.v1i1.69.

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ABSTRAK Sejalan dengan peningkatan sumber daya dan cadangan emas-perak di PT. Agincourt Resources (PTAR) dari tahun 2017-2018 dan mengkaji fasilitas penyimpanan tailing yang ada saat ini diperhitungkan tidak mampu menampung peningkatan volume tailing sehingga dilakukan penentuan lokasi yang baru. Pemilihan beberapa lokasi baru untuk fasilitas ini sudah dimulai sejak pertengahan tahun 2018 dan Departemen eksplorasi bekerja sama dengan Departemen project development ditugaskan untuk menyelidiki bahwa daerah yang dipilih adalah lokasi yang sesuai. Pengeboran dan data IP (Induced Polarisation) geofiska, digunakan untuk menentukan apakah lokasi yang diusulkan merupakan lokasi yang steril dari sumber daya mineral ekonomis dan stabil secara geoteknik. Program pengeboran fase pertama sudah selesai pada Q1 tahun 2019, berdasarkan data geology permukaan, geokimia dan geofisika yang sudah ada sebelumnya. Limabelas titik bor dengan total kedalaman 6.802m telah dilakukan di daerah rencana dengan rata-rata total kedalaman 500 meter. Data geologi, struktur dan geokimia bawah permukaan yang diperoleh dari hasil pengeboran akan dikaji untuk menentukan apakah lokasi yang dipilih tepat dan cocok untuk fasilitas tailing manajemen. Fase pengeboran tahap 2 atau tindak lanjut sedang dilakukan, namun tergantung dari hasil survei IP 3D yang baru saja selesai dan saat ini juga sedang dilakukan pemodelan hasil pembacaan geofisika berupa data resistivitas dan chargeabilitas (jika ada indikasi anomali) di area yang belum dilakukan pengeboran sebelumnya, untuk memastikan bahwa area tersebut steril atau tidak terdapat mineral ekonomis. Ketersediaan data teknis dari program eksplorasi juga dapat digunakan untuk mendukung pekerjaan di departemen lain dan hal ini menguntungkan secara signifikan untuk penghematan biaya serta dapat memastikan bahwa pekerjaan selain geologi tidak mempengaruhi potensi/target eksplorasi di daerah tersebut dan memberikan gambaran untuk perencanaan pengeboran lebih lanjut untuk kondisi geoteknik setempat. Kata Kunci: IP Survei, chargeabilitas, geoteknik, geofisika, mineral ABSTRACT As a consequence of an increase in resources and reserves at the Martabe Gold Mine in 2017-2018 the current tailings management facility will be unable to handle the additional tailings and therefore a new location is being pursued. The selection of several new locations for this facility began in mid-2018 and the exploration department in collaboration with the project development department was tasked with investigating that the area chosen was the appropriate location. Drilling and IP (Induced Polarisation) geophysical data was used to determine if the proposed location is likely to contain any significant economic mineralisation and is geotechnically stable.A first phase drilling program that was based on historical surface geology, geochemical and geophysics data was completed in Q1 of 2019. Fifteen drill holes with total of 6,802m were collared within or proximal to the proposed location and were drilled to an average depth of 500m. Subsurface geology, structure and geochemical data acquired in the Phase 1 drilling program was reviewed to determine if the area was suitable for facility tailings management. A second or follow up drilling phase is being considered but is dependent on the results of a recently completed 3D IP survey that is currently being modelled which will provide resistivity and chargeability geophysical signatures (if any) over the area not yet drill tested to ensure that the area is sterile of economic mineralisation. The availability of technical data from Exploration programs being made available to other departments can be significant for cost saving measures and ensure that non geological projects do not affect the exploration potential in the district and provide an overview for further drill planning for geotechnical conditions. Keywords: IP Survey, chargeability, geotechnical, geophysics, mineral
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Favier, Philomène, Alan Poulos, Jorge Andrés Vásquez, Paula Aguirre, and Juan Carlos de la Llera. "Seismic Risk Assessment of an Emergency Department of a Chilean Hospital Using a Patient-Oriented Performance Model." Earthquake Spectra 35, no. 2 (May 2019): 489–512. http://dx.doi.org/10.1193/103017eqs224m.

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After an earthquake, hospital emergency departments need to provide continuous health care services to respond to the eventual sudden increase in injured people. The service performance of an emergency department is influenced by internal factors, such as physical damage and staff availability, and external factors, such as an increased patient arrival rate and disruptions in its supply chain. This research presents a quantification methodology for the performance of the emergency department. The novelty of the proposed approach lies in the explicit integration of the inelastic structural and nonstructural response of the building and damage with its loss of functionality, downtime, and emergency patient treatment rate. A discrete event simulation model is used to model the flow of patients within the different units of the emergency department. The seismic risk is expressed as return periods of exceeding different levels of patient waiting times. Results show that 1,000 and 30,000 accumulated waiting hours correspond to return periods of 100 and 1,000 years, respectively. It is concluded that this model may contribute to improving the risk management of critical emergency department infrastructure.
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Crabb, T. N., and P. R. Dunne. "Environmental Impact of Seismic Exploration Activities in Pels 5 & 6, Sa – A Department of Mines and Energy Perspective." Exploration Geophysics 22, no. 1 (March 1991): 85–92. http://dx.doi.org/10.1071/eg991085.

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Papadopoulos, T. D., N. Goulty, N. S. Voulgaris, J. D. Alexopoulos, I. Fountoulis, P. Kambouris, V. Karastathis, et al. "Tectonic structure of Central-Western Attica (Greece) based on geophysical in vestigations-Preliminary results." Bulletin of the Geological Society of Greece 40, no. 3 (June 5, 2018): 1207. http://dx.doi.org/10.12681/bgsg.16873.

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In an effort to investigate the deep geological structure in the broader area of central-western Attica, that suffered severe damage during the destructive Athens earthquake of September 7th, 1999, the Department of Geophysics-Geothermics of the Faculty of Geology and Geoenvironment of Athens University, in collaboration with the Geodynamic Institute of National Observatory of Athens and the Department of Geological Sciences of Durham University, carried out a combined geophysical survey. For the first time in Attica, seismic and gravity geophysical methods were applied along profiles, in such an extensive scale. Within the framework of this investigation the following tasL· were accomplished: a) Three (3) seismic lines of about 30 kilometres of total length, two (2) in the area of Thriassion plain and one (1) along the Parnitha-Krioneri-Drosia-Ekali-Dionysos axis (Attica plain) and b) 338 gravity measurements distributed along eight (8) gravity profiles, four (4) of which in Thriassion plain, three (3) in Petroupoli-Aharnes-Thrakomakedones region (Attica plain) and one (1) along Parnitha-Krioneri-Drosia-Ekali-Dionysos axis (Attica plain). Preliminary results of the geophysical investigation combined with existing geological and tectonic data are presented in this paper. Significant variation in the elevation of the alpine basement has been detected, expressed by manifestation of low and high subsurface areas which are well correlated with existing fault zones. In the area of Thriassion plain the thickness of post-alpine sediments is estimated of a few hundred meters (<500 meters) and huge thickness of several hundred meters (-800 meters) of post-alpine sediments were detected in Thrakemakedones and Krioneri areas. The relief of alpine basement is more intense in fault zones areas, such as Thriassion plain (WNW-ESE), Pathitha and Kifissos (NE-SW) as well as along the fault zone outline the Fili and Aharnes graben and is covered by postalpine formations
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Cassiliano, Michael. "Online specimen catalog available at the University of Wyoming." Journal of Paleontology 76, no. 1 (January 2002): 194. http://dx.doi.org/10.1017/s0022336000017492.

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The specimen catalogue of the Collection of Fossil Vertebrates in the Department of Geology and Geophysics at the University of Wyoming in Laramie is now available on the World Wide Web. The URL for the site is http://paleo.gg.uwyo.edu. The construction of the website is the final step in the collection improvement grant (DBI-9808626) awarded by the National Science Foundation to Jay Lillegraven and Mike Cassiliano. The website was built by Brian Kraatz, a graduate student of Jay's. The specimen catalogue lists over 41,000 vertebrate fossils, an increase of more than 14,000 since the start of the grant. The collection's main focus is on mammals from the late Cretaceous, Paleocene, and early Eocene.
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McCormack, Thomas C., and Franz N. Rad. "An Earthquake Loss Estimation Methodology for Buildings Based on ATC-13 and ATC-21." Earthquake Spectra 13, no. 4 (November 1997): 605–21. http://dx.doi.org/10.1193/1.1585971.

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A survey of the seismic hazards for about 30,000 nonresidential buildings in Portland, Oregon was conducted, and an earthquake damage and loss estimation model was developed. To conduct the buildings survey, ATC-21's Rapid Screening Procedure was used. For each building the data included: address, year built, area, number of stories, building name, use, occupancy type, estimated range of number of people, nonstructural falling hazards, building type, and performance modifiers such as soft story and torsion. Soil data were provided by the Earthquake Hazard Maps published by the Oregon Department of Geology and Mineral Industries. The algorithm set up on the GIS was to compute the structural score based on ATC-21 score, modify the score based on the geologic condition of the site, and finally, compute the damage. The proposed loss estimation model is based on ATC-13, and the scoring system developed by ATC-21. The results are in terms of percent (or dollar) damage to buildings in the survey and loss of life and serious injuries.
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Harper, F. "Undiscovered oil and gas resources: An evaluation of the department of the interior's 1989 assessment procedures." Marine and Petroleum Geology 9, no. 6 (December 1992): 673. http://dx.doi.org/10.1016/0264-8172(92)90041-c.

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Yurek, Peter, Stuart McKernan, and Kyung-Ho Lee. "The Construction of an EBSD Stage for the Electroscan E3 SEM." Microscopy and Microanalysis 6, S2 (August 2000): 796–97. http://dx.doi.org/10.1017/s1431927600036473.

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With recent advances in computing power and application specific software it has become practical for smaller microcopy labs to either purchase or build a electron backscatter diffraction (EBSD) systems. This system can be used to probe the crystallography and microstructure of many different materials. One set of such materials is geological samples from deep within the earth's crust. In collaboration with the Geology and Geophysics department an EBSD system has been built to function with the Philips Electroscan E3 Environmental Scanning Electron Microscope (ESEM). Using an existing low light level SIT camera, the system was completed with the addition of a phosphor screen and appropriate software and acquisition cards.One main advantage of the ESEM for EBSD is that since it is an environmental SEM samples can be imaged without coating. For insulating materials this is means that the sample can be imaged without coating.
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Dissertations / Theses on the topic "Department of Geology and Geophysics"

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Garrick-Bethell, Ian 1980. "Early lunar geology and geophysics." Thesis, Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1721.1/47845.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2009.
Includes bibliographical references.
Despite a number of human and robotic missions to the Moon, there are still important unanswered questions about its early evolution, and how it came to be the object we observe today. Here we use observational, experimental, and theoretical techniques to examine three important events that took place early in lunar history and have left a lasting signature. The first event is the formation of the largest basin on the Moon, the South Pole-Aitken Basin. We develop a systematic method to define the previously unknown boundaries of this degraded structure and quantify its gross shape. We also combine a number of remote sensing data sets to constrain the origin of heat producing elements in its interior. The second event we examine is the evolution of the lunar orbit, and the coupling between the Moon's early geophysical properties and the growth of orbital eccentricity. We use analytical models for tidal deformations and orbit evolution to show that the shape of the Moon suggests its early orbit was highly eccentric. However, we are also able to explain the presently high eccentricity entirely by traditional, secular tidal growth while the early Moon was hot. The third event we examine is the magnetization of lunar samples. We perform extensive paleomagnetic measurements of an ancient, deep-seated lunar sample, and determine that a long-lived magnetic field like that of a core dynamo is the most plausible explanation for its magnetic remanence. In sum, the earliest portion of lunar history has been largely obscured by later geologic events, but a great deal can still be learned from this formative epoch.
by Ian Garrick-Bethell.
Ph.D.
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Seiler, Christina. "Structural and thermal evolution of the Gulf Extensional Province in Baja California, Mexico : implications for Neogene rifting and opening of the Gulf of California /." Connect to thesis, 2009. http://repository.unimelb.edu.au/10187/4212.

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Everett, Keith R. "USW area analogs." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Jun%5FEverett.pdf.

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Thesis (M.S. in Meteorology and Physical Oceanography)--Naval Postgraduate School, June 2005.
Thesis Advisor(s): D. Benjamin Reeder, Mary Batteen. Includes bibliographical references (p. 119-121). Also available online.
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Abbas, Mazin Y. "Incorporating seismic attribute variation into the pre-well placement workflow, a case study from Ness County, Kansas, USA." Thesis, Kansas State University, 2009. http://hdl.handle.net/2097/1658.

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Master of Science
Department of Geology
Matthew W. Totten
3D seismic surveys have become the backbone of many exploration programs because of their high resolution and subsequent success for wildcat test wells. There are occasions when the predicted subsurface geology does not agree with the actual geology encountered in the drilled well. A case in point occurred during the drilling of several wells based upon a 3D seismic survey in Ness County, Kansas, where the predicted Cherokee Sand did not meet the expectations. By better understanding the subsurface geologic features in the subject area, this study will attempt to answer the question “what went wrong?” Seismic attribute analysis workflow was carried out and the results were correlated to the available geological and borehole data within the survey boundaries. The objective of running this workflow was to describe facies variations within the Cherokee Sandstone. Correlations between seismic attributes and physical properties from well data were used to define these variations. Finally, Distributions of the seismic facies were mapped to predict the distribution of potential reservoir rocks within the prospect area.
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Fried, Mason. "Grounding Zone Process| Ice Mechanics and Margin Lakes, Kamb Ice Stream and Whillans Ice Stream, West Antarctica." Thesis, Portland State University, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1542719.

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The lateral "corners" where Kamb and Whillans Ice Streams (KIS and WIS) discharge into the Ross Ice Shelf share common geometries and ice mechanical settings. At both corners of the now-stagnant KIS outlet, shear margins of apparently different ages confine regions with a relatively flat, smooth surface expression. These features are called the "Duckfoot" on the northern, right-lateral side and the "Goosefoot" on the other. It has been suggested, on evidence found in ice internal layers, that the flat ice terrains on KIS were afloat in the recent past, at a time when the ice stream grounding line was upstream of its present location. The overdeepening in the bed just upstream of the KIS grounding line supports this view of the past geometry.

The right-lateral margin at the outlet of the currently active WIS, the location of Subglacial Lake Englehardt (SLE), appears to have many similarities with the right lateral margin of KIS, though with a less developed looking inboard margin. This paper presents a mechanical analysis using surface and bed topography and velocity datasets comparing the Duckfoot flat ice terrain with the terrain around Subglacial Lake Englehardt. At both locations mechanical thinning along shear margins and lows in the bed topography redirects basal water routing towards the features. Here, I consider the history of these features and their role in ice stream variability by comparison of the relict and modern features and via numerical modeling of ice shelf grounding and ungrounding in response to variations in ice flow.

We propose two scenarios for the development of flat ice terrains/subglacial lakes at the outlets of ice streams. In the first, development of a lake in the hydraulic potential low along a shear margin forces a margin jump as shearing develops along the inboard shore of the margin lake. This thesis presents evidence for an inboard (relative to the main outboard shear margin) zone of shear along the inboard shoreline of SLE, suggesting that subglacial lakes along shear margins are capable of facilitating shear margin jumps. In the second, grounding line advance around a relative low in the bed, creating adjacent margins along the lakeshores, forms a remnant lake. Discerning which of these scenarios is appropriate at the KIS outlet has implications for understanding the history of the ice stream grounding line.

An ice flow model is used to place these local conditions in a regional context by studying the effect of internal perturbations, such as ice rise stagnation or inward margin jumps, on grounding line position. Bathymetry is important in determining ice stream flow in the ways that might not be otherwise realized in 1-D flow model studies. In the numerical modeling experiments, grounding line advance across the KIS outlet is mediated by the overdeepening in the bed and proceeds not in the direction of ice flow but transverse to flow. This finding adds complexity to both a flowline view of grounding line migration and the theory that grounding lines are unstable in the presence of inward sloping bed topography.

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Bellefontaine, Kim Angelina. "The tectonic evolution of the Ingenika group and its implications for the boundary between the Omineca and Intermontane belts, north-central British Columbia /." Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59960.

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The Ingenika Range forms part of a large zone of structural divergence that roughly coincides with the boundary between North America and Superterrane I. Contrasting tectonic histories from the Intermontane, Omineca and Foreland Belts at the latitude of the thesis area are consistent with a collisional model involving tectonic wedging, delamination and large-scale backthrusting.
The Upper Proterozoic Ingenika Group in the Ingenika Range has undergone a progressive deformational history involving pre-, syn-, and post-metamorpic structures. During the Middle Jurassic regional structural vergence changed from northeast- to southwest-directed folds and faults. Regional metamorphism reached amphibolite grade and was synchronous with west-vergent deformation. Minor structures in the study area suggest that the Swannell fault was an east-dipping thrust fault that emplaced North American strata over allochthonous rocks of Quesnellia. The Swannell fault was probably also active during the Middle Jurassic and may have acted as the structural discontinuity between a backthrusted crustal flake and an underlying, eastward moving wedge.
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Karavas, Costas. "Fractal chaotic systems : investigation of the geological system and its sedimentation behaviour." Thesis, McGill University, 1990. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60052.

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Chaos theory has only recently been related to various phenomena in the earth sciences. Here, using systems theory in a description of geological processes, we study the chaotic development of sedimentary sequences.
The geosystem is treated as a partially specified system in order to apply qualitative stability analysis in the investigation of sedimentation behaviour and interactions among geological processes. The analysis suggests that the sedimentary system is unstable. This instability in conjunction with the system's sensitive dependence to internal fluctuations (i.e., those generated within the system) provide supporting evidence to suggest a chaotic behaviour for the sedimentation system.
We suggest that chaos could act as the common underlying mechanism which is manifest as the fractal-flicker noise character observed in reflectivity well logs. Acoustic impedance variations--the geophysical measures of lithologic variability--represent the internal organization of the interacting geological processes. This organization under a chaotic regime is responsible for the common statistical character found in various sedimentary basins.
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Ghods, Abdolreza. "Melt migration modeling in partially molten upper mantle." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0024/NQ50169.pdf.

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Hegmann, Mary Jane. "Gravity and magnetic surveys over the Santa Rita Fault System, southeastern Arizona." Thesis, The University of Arizona, 1998. http://hdl.handle.net/10150/278675.

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Gravity and magnetic surveys were performed in the northeast portion of the Santa Rita Experimental Range, in southeastern Arizona, to identify faults and gain a better understanding of the subsurface geology. A total of 234 gravity stations were established, and numerous magnetic data were collected with portable and truck-mounted proton precession magnetometers. In addition, one line of very low frequency electromagnetic data was collected together with magnetic data. Gravity anomalies are used to identify two normal faults that project northward toward a previously identified fault. The gravity data also confirm the location of a second previously interpreted normal fault. Interpretation of magnetic anomaly data indicates the presence of a higher-susceptibility sedimentary unit located beneath lower-susceptibility surficial sediments. Magnetic anomaly data identify a 1-km-wide negative anomaly east of these faults caused by an unknown source and reveal the high variability of susceptibility in the Tertiary intrusive rocks in the area.
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Dupont-Nivet, Guillaume. "Constraints on the mechanism of the Altyn Tagh fault from paleomagnetism." Diss., The University of Arizona, 2002. http://hdl.handle.net/10150/280011.

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First, paleomagnetic data were obtained from Tertiary red beds at two localities separated by several hundred kilometers within the Qaidam Basin. When compared with equivalent-age expected directions for Eurasia, the mean paleomagnetic directions indicate no Neogene vertical-axis rotation of the Qaidam Basin or the Altyn Tagh fault. The Qaidam Basin may act as an indentor translating without rotation toward the Sino-Korean craton. Second, the observed paleomagnetic direction from Miocene red beds in the central Tarim Basin indicates 30.8° ± 5.5° flattening of inclination and 15.3° ± 6.7° clockwise vertical-axis rotation. Anisotropy of magnetic susceptibility measurements indicate a rock-magnetic (depositional or compaction shallowed) origin for the inclination flattening. Local deformation is the preferred interpretation for the vertical-axis rotation. Third, paleomagnetic data were obtained along the arcuate Tula syncline to test whether its strike curvature is due to oroclinal bending. The observed 13.3° ± 8.8° declination difference between the two halves of the Tula syncline is far less than the ∼40° difference predicted by oroclinal bending. Instead the arc shape of the syncline is an original configuration produced by transport above an arcuate thrust ramp. Along with paleomagnetic data from the Qaidam Basin, this result indicates that crustal displacement between the Tarim Basin and the Tibetan Plateau is accommodated by strike-slip motion on the Altyn Tagh fault rather than distributed shear within the northern Tibetan Plateau. Finally, we present results from red beds in the Altun Shan, the Qilian Shan/Nan Shan fold-thrust-belt and the Hexi corridor. In the Altun Shan, results from Miocene beds indicate no significant vertical-axis rotation confirming that the Altyn Tagh fault has not rotated and that sinistral shear strain is concentrated on the fault. Paleomagnetic results from Nan Shan/Qilian Shan fold-thrust-belt indicate no rotation since 30 Ma contrasting with prediction from previous kinematic models. This result indicates that there is no transrotation of the belt associated with motion on the Altyn Tagh fault. In the Hexi corridor, the observed mean paleomagnetic direction is concordant with the expected direction at 110 Ma providing a new local paleomagnetic reference for the Sino-Korean craton in agreement with published reference paleomagnetic poles for Eurasia.
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Books on the topic "Department of Geology and Geophysics"

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Burgh, Christine L. Van. Bibliography and index of graduate theses and dissertations of the Department of Geology and Geophysics, University of Wyoming. Laramie, Wyo. (P.O. Box 3008, University Sta., Laramie 82071-3008): Geological Survey of Wyoming, 1989.

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Convention and Seminar on Exploration Geophysics (13th 1987 Dept. of Geology, M.S. University). Souvenir, thirteenth annual Convention and Seminar on Exploration Geophysics, 12th-14th November, 1987, Department of Geology, M.S. University, Baroda, Gujarat: Special theme, integrated geophysical exploration for mineral deposits. Edited by Sreedhar Murthy Y, Association of Exploration Geophysicists. Convention, Maharaja Sayajirao University of Baroda., and India Oil and Natural Gas Commission. [Hyderabad, India]: Association of Exploration Geophysicists, 1987.

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Quantitative geophysics and geology. London: Springer, 2000.

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W, Coates Robert, ed. The lithosphere: Geochemistry, geology and geophysics. Hauppauge, N.Y: Nova Science Publishers, 2008.

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Dmowska, Renata. Advances in geophysics. Amsterdam: Elsevier/Academic Press, 2008.

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Fractals and chaos in geology and geophysics. 2nd ed. Cambridge, U.K: Cambridge University Press, 1997.

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Fractals and chaos in geology and geophysics. Cambridge: Cambridge University Press, 1992.

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Environmental and engineering geophysics. Cambridge, U.K: Cambridge University Press, 1997.

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Henry, Georges. Geophysics for sedimentary basins. Paris: Editions Technip, 1997.

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Sari, Driss Ben. Connaissance géophysique du Maroc. Rabat: Editions du Service géologique du Maroc, 1988.

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Book chapters on the topic "Department of Geology and Geophysics"

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Turcotte, Donald L. "Fractals in Geology and Geophysics." In Fractals in Geophysics, 171–96. Basel: Birkhäuser Basel, 1989. http://dx.doi.org/10.1007/978-3-0348-6389-6_10.

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Todoeschuck, J. P., and O. G. Jensen. "Scaling Geology and Seismic Deconvolution." In Fractals in Geophysics, 273–87. Basel: Birkhäuser Basel, 1989. http://dx.doi.org/10.1007/978-3-0348-6389-6_15.

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Turcotte, Donald L. "Fractals in Geology and Geophysics." In Mathematics of Complexity and Dynamical Systems, 532–36. New York, NY: Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-1806-1_33.

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Turcotte, Donald L. "Fractals in Geology and Geophysics." In Encyclopedia of Complexity and Systems Science, 3822–26. New York, NY: Springer New York, 2009. http://dx.doi.org/10.1007/978-0-387-30440-3_224.

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Turcotte, Donald L. "Fractals in Geology and Geophysics." In Extreme Environmental Events, 568–72. New York, NY: Springer New York, 2011. http://dx.doi.org/10.1007/978-1-4419-7695-6_31.

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Planke, Sverre, Henrik Svensen, Reidun Myklebust, Stephen Bannister, Ben Manton, and Lars Lorenz. "Geophysics and Remote Sensing." In Physical Geology of Shallow Magmatic Systems, 131–46. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/11157_2014_6.

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Planke, Sverre, Henrik Svensen, Reidun Myklebust, Stephen Bannister, Ben Manton, and Lars Lorenz. "Geophysics and Remote Sensing." In Physical Geology of Shallow Magmatic Systems, 131–46. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-14084-1_6.

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Aldrich, L. T. "Isotope geology at Carnegie 1950–1970: Dating Earth processes." In History of Geophysics, 215–23. Washington, D. C.: American Geophysical Union, 1994. http://dx.doi.org/10.1029/hg005p0215.

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Todoeschuck, John P. "Fractals and Exploration Geophysics." In Fractals in Petroleum Geology and Earth Processes, 295–314. Boston, MA: Springer US, 1995. http://dx.doi.org/10.1007/978-1-4615-1815-0_14.

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Todoeschuck, J. P., and O. G. Jensen. "1/f Geology and Seismic Deconvolution." In Non-Linear Variability in Geophysics, 261–68. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2147-4_20.

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Conference papers on the topic "Department of Geology and Geophysics"

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E. Campbell, A., B. C. Scheffers, and P. F. M. de Groot. "Geophysics - Desperately seeking geology." In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410261.

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Guillen, A. "Inverse Problem Using Geology and Geophysics." In EAGE/SPE Joint Workshop on Beyond Closed Loop Integrated Monitoring. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20132054.

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Lobankov, V. M., and V. Sviatokhin. "Measurements in Petroleum Geology and Geophysics." In 6th Saint Petersburg International Conference and Exhibition. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140244.

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Witherly, Ken. "Integrating geophysics and geology in 3D." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059128.

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Taylor, J., T. Jones, C. Allen, D. Griffin, A. Campbell, E. Ferguson, J. Huff, and M. Mahnke. "Validaing a Borehole Seismic Survey in Complex Geology." In 3rd EAGE Workshop on Borehole Geophysics. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201412186.

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Mascle, J., and E. Chaumillon. "Marine Geology and Geophysics of the Eastern Mediterranean." In 5th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1997. http://dx.doi.org/10.3997/2214-4609-pdb.299.30.

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Grimston, O. G., and P. A. Connolly. "Bed Thickness Distributions - The Geology Behind the Geophysics." In 76th EAGE Conference and Exhibition 2014. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20141626.

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Al-Atroshi, K., Tan Ching Kiang, and Amri Amdan. "Analytical Review of Hamrong Geology and Geophysics Data." In First EAGE South-East Asia Regional Geology Workshop - Workshop on Palaeozoic Limestones of South-East Asia and South China. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144019.

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Slepak, Z. M. "Near Surface Geophysics in Engineering Geology and Archeology." In Saint Petersburg 2012. Netherlands: EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143695.

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Wilbur, Bryan C. "WORK HARD, PLAY HARD: THE VALUE OF A GEOLOGY CLUB TO A TWO-YEAR COLLEGE GEOLOGY DEPARTMENT." In 116th Annual GSA Cordilleran Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020cd-347050.

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Reports on the topic "Department of Geology and Geophysics"

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Sanford, B. V., G. B. J. Fader, and P. N. Moir. Regional geology and geophysics 8: bedrock geology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210609.

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Hamilton, T. S. Georgia Basin: Submarine Geology and Geophysics. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131179.

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Shih, K. G., R. Macnab, S. D. Dods, and J. Woodside. Regional geology and geophysics 1: magnetic anomaly. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210591.

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Shih, K. G., R. Macnab, R. K. McConnell, D. B. Hearty, J F Halpenny, and J. Woodside. Regional geology and geophysics 2: gravity anomaly. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210592.

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Srivastava, S. P., S. Levesque, W. R. Roest, and J. Verhoef. Regional geology and geophysics 5: plate reconstructions, bathmetry. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210595.

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Solie, D. N., and L. E. Burns. Alaska GeoSurvey News - Alaska Highway corridor geology and geophysics. Alaska Division of Geological & Geophysical Surveys, March 2007. http://dx.doi.org/10.14509/15756.

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Kay, W., B. C. MacLean, and C. E. Keen. Regional geology and geophysics 3: Nova Scotian margin crustal transect. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210593.

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Pelletier, B. R. Marine science atlas of the Beaufort Sea: geology and geophysics. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/126940.

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Tschirhart, Lori. Geophysics and Seismology / Structural Geology and Neotectonics - University of Michigan. Purdue University Libraries, September 2012. http://dx.doi.org/10.5703/1288284315004.

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Bell, J. S., and J. Adams. Regional geology and geophysics 4: crustal stresses, earthquakes and crustal thickness. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210594.

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