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Relevant bibliographies by topics / Sedimentary terrain

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Academic literature on the topic 'Sedimentary terrain'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Sedimentary terrain"

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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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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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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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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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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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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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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 BinduraShamva 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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Dissertations / Theses on the topic "Sedimentary terrain"

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Kemp, A. E. S. "The later (Silurian) sedimentary and tectonic evolution of the Southern Uplands accretionary terrain." Thesis, University of Edinburgh, 1985. http://hdl.handle.net/1842/15143.

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Blanchet, François. "Etude géomécanique de glissements de terrain dans les argiles glacio-lacustres de la vallée du Drac." Phd thesis, Grenoble 1, 1988. http://www.theses.fr/1988GRE10117.

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Nous avons etudie un glissement de terrain affectant le lotissement du mas d'avignonet, situe sur la rive gauche de la retenue du monteynard. Une campagne de reconnaissance in situ comportant sondages, releves geologiques, indices de mouvement, mesures inclinimetriques, topographiques et piezometriques nous a permis de mettre en evidence plusieurs surfaces de deformations. On propose des mecanismes probables de rupture de ces glissements; on definit leur geometrie et on evalue les valeurs residuelles des caracteristiques mecaniques a la rupture des argiles litees, formation a l'origine de nomb

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Saporetti, Camila Martins. "Comparação de técnicas de inteligência computacional para classificação de dados petrográficos." Universidade Federal de Juiz de Fora (UFJF), 2016. https://repositorio.ufjf.br/jspui/handle/ufjf/3542.

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Submitted by Renata Lopes (renatasil82@gmail.com) on 2017-03-03T18:03:20Z No. of bitstreams: 1 camilamartinssaporetti.pdf: 9003270 bytes, checksum: e53ab03d47e88504332820b3ae1956a3 (MD5)<br>Approved for entry into archive by Adriana Oliveira (adriana.oliveira@ufjf.edu.br) on 2017-03-06T20:17:46Z (GMT) No. of bitstreams: 1 camilamartinssaporetti.pdf: 9003270 bytes, checksum: e53ab03d47e88504332820b3ae1956a3 (MD5)<br>Made available in DSpace on 2017-03-06T20:17:46Z (GMT). No. of bitstreams: 1 camilamartinssaporetti.pdf: 9003270 bytes, checksum: e53ab03d47e88504332820b3ae1956a3 (MD5) Previ

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Miranda, Gasca Miguel Angel. "The volcanogenic massive sulfide and sedimentary exhalative deposits of the Guerrero Terrane, Mexico." Diss., The University of Arizona, 1995. http://hdl.handle.net/10150/187087.

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More than 60 volcanogenic massive sulfide and sedimentary exhalative deposits are located in the composite upper Jurassic-lower Cretaceous Guerrero terrane of western Mexico. The deposits range from less than 100,000 metric tons up to 6 million metric tons. Most of the deposits are Zn-Pb-Cu Kuroko type and are located within the Zihuatanejo and Teloloapan subterranes. The Guanajuato and Calmalli, Baja California, deposits are Zn-Cu. The Cu type Copper King, Guerrero, deposit is located in the Papanoa complex. Arroyo Seco, Michoacan, is the only Pb-type and can be classified as a sedimentary-ex

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Le, Bouteiller Pauline. "Identification and characterization of Mass Transport Deposits from seismic data. Application to the Amazon River Mouth basin." Electronic Thesis or Diss., Sorbonne université, 2018. http://www.theses.fr/2018SORUS481.

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Comprendre les processus ayant engendré un « Mass Transport Deposit » (MTD) permet une meilleure connaissance des ressources potentielles d’un bassin sédimentaire et de l’aléa glissement de terrain sous-marin. L’interprétation de données sismiques est abordée pour étudier les MTDs. Deux méthodologies sont développées dans cette thèse, pour inférer les processus physiques ayant impacté l’aspect actuel de MTDs dans des images sismiques. La méthodologie d’ « identification » de MTDs dans des images sismiques s’attache à déterminer la position et les contours de ces objets géologiques tout en prés

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Silva, Cláudia Alexandra Fernandes. "Dinâmica sedimentar em sistemas dunares litorais. Aplicação ao sistema dunar da praia do Guincho, Cascais." Master's thesis, ISA/UL, 2015. http://hdl.handle.net/10400.5/11160.

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Mestrado em Arquitectura Paisagista - Instituto Superior de Agronomia<br>The Guincho's beach dune system is part of a larger system, called Guincho-Oitavos's dune system. This is one of the most remarkable wind corridors of the European continent, and is extremely important for our natural heritage. However, the anthropogenic activity has been causing changes in its natural evolution process, destabilizing it. In this dissertation it's analyzed the development of Guincho's beach dune system in recent years, and it's also developed a theoretical exercise that estimates its possible future

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Oliveira, Álvaro Filipe Monteiro. "Estudo dos depósitos lutíticos da orla ocidental: matérias-primas minerais." Doctoral thesis, Universidade de Aveiro, 2010. http://hdl.handle.net/10773/3635.

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Doutoramento em Geociências<br>Neste trabalho foram efectuados estudos de natureza químico – mineralógica e tecnológica em quatro depósitos sedimentares: Vale Grande, Aguada de Cima, Anadia e Monsarros. Estes estudo permitiram o estabelecimento da coluna tipológica em cada um dos depósitos. No jazigo de Aguada evidencia-se a existência de dois níveis argilosos: a unidade “Barro Negro” de natureza ilito-quartzo-caulinítica (argilas especiais) e a unidade “Argilas de Boialvo” com composição quartzo – ilite – caulinite (argilas comuns). Nos jazigos de Anadia e Monsarros o enchimento argil

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Souza, Flavo Elano Soares de. "Evolu??o morfodin?mica da regi?o de influ?ncia estuarina do Rio Curimata?/RN, com ?nfase nas alternativas do ambiente deposicional de manguezal e a integra??o de geodados em Sig." Universidade Federal do Rio Grande do Norte, 2004. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18358.

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Made available in DSpace on 2015-02-24T19:48:41Z (GMT). No. of bitstreams: 1 FlavoESS.pdf: 7200814 bytes, checksum: 50030d58571208fd3287ef1805413e5f (MD5) Previous issue date: 2004-04-07<br>Conselho Nacional de Desenvolvimento Cient?fico e Tecnol?gico<br>The estuaries are important investigation zones of the actual morphodynamic and of depositional facies of recent geological history. They are constituted in important receptor means of the coastal area sediments, where the evolutionary processes occur quickly. They are also attractive means for the development of anthropic activities, which

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Aichholzer, Coralie. "Le log complet de la stratigrahie de la zone rhénane ainsi que les modilités stratigraphiques, sédimentaires et structurales de la transition socle-couverture : application à la géothermie profonde." Thesis, Strasbourg, 2019. http://www.theses.fr/2019STRAH008/document.

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Depuis la mise en place en 2010, d’une nouvelle tarification française sur le tarif de l’énergie géothermique, l’Alsace est la région de France la plus dynamique quant à la réalisation de forages géothermiques profonds à haute température (>150°C). Ainsi, l’approche géologique, qui a été primordiale pour les forages de Rittershoffen, le sera encore davantage pour les projets à venir compte tenu de la méconnaissance géologique de certaines zones profondes du bassin rhénan. Cette étude propose d’appréhender la compréhension de l’architecture stratigraphique et séquentielle des formations de l

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Sousa, Thiago Andrade de. "Elementos terras raras como indicadores do aporte e proveniência sedimentar nos últimos 45 mil anos, Bacia e Santos - Brasil." Niterói, 2017. https://app.uff.br/riuff/handle/1/3269.

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Submitted by Biblioteca de Pós-Graduação em Geoquímica BGQ (bgq@ndc.uff.br) on 2017-04-03T16:44:03Z No. of bitstreams: 1 THIAGO ANDRADE DE SOUSA .pdf: 5768772 bytes, checksum: b3c4e1c52ed521e2c3772627711af6fa (MD5)<br>Made available in DSpace on 2017-04-03T16:44:03Z (GMT). No. of bitstreams: 1 THIAGO ANDRADE DE SOUSA .pdf: 5768772 bytes, checksum: b3c4e1c52ed521e2c3772627711af6fa (MD5)<br>Coordenação de Aperfeiçoamento de Pessoal de Nível Superior<br>Universidade Federal Fluminense. Instituto de Química. Programa de Pós-Graduação em Geociências- Geoquímica Ambiental. Niterói, RJ<br>Os

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Books on the topic "Sedimentary terrain"

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Tucker, Maurice E. Sedimentary rocks in the field: A practical guide. 4th ed. Wiley, 2011.

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Sedimentary Rocks in the Field. Wiley & Sons, Incorporated, John, 2003.

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Tucker, Maurice E. Sedimentary Rocks in the Field. Wiley & Sons, Incorporated, John, 2011.

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Tucker, Maurice E. Sedimentary Rocks in the Field: A Practical Guide. Wiley & Sons, Incorporated, John, 2011.

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Tucker, Maurice E. Sedimentary Rocks in the Field: A Practical Guide. Wiley & Sons, Incorporated, John, 2011.

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Tucker, Maurice E. Sedimentary Rocks in the Field: A Practical Guide. Wiley & Sons, Incorporated, John, 2011.

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Book chapters on the topic "Sedimentary terrain"

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Chandrajith, R., S. Diyabalanage, and C. B. Dissanayake. "Sources and mobilization of geogenic arsenic in groundwater in a sedimentary terrain of Sri Lanka." In Arsenic in the Environment: Bridging Science to Practice for Sustainable Development As2021. CRC Press, 2024. http://dx.doi.org/10.1201/9781003317395-59.

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Németh, Károly. "Volcanic Geoheritage in the Light of Volcano Geology." In Geoheritage, Geoparks and Geotourism. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07289-5_1.

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AbstractVolcanic geoheritage relates to the geological features of a region that are associated with the formation of a volcanic terrain in diverse geoenvironmental conditions. These features include the volcanic processes, volcanic landforms and/or the eruptive products of volcanism that form the geological architecture of that region. Volcanic geoheritage is expressed through the landscape and how it forms and evolves through volcanic processes on various spatio-temporal scales. In this sense it is directly linked to the processes of how magma released, transported to the surface and fragmen

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Di Paola, Gianluigi, Grazia Dilauro, Claudia Caporizzo, and Carmen M. Rosskopf. "Monitoring beach erosion along the Central Adriatic coast: the case study of Molise Region." In Monitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques. Firenze University Press, 2024. https://doi.org/10.36253/979-12-215-0556-6.62.

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Coastal areas characterized by sandy shorelines are among the most dynamic environments and subject to deep and rapid changes over time under the influence of natural and anthropic factors. Therefore, reconstructing the geomorphological and anthropogenic evolution, current state and possible near-future trends of a sandy beach is essential for deepening the understanding of its potential future development and better outlining measures for its sustainable management. Therefore we have examined the coast of the Molise Italy, which is predominantly made of sandy shorelines and characterized by w

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Steidtmann, James R., and James G. Schmitt. "Provenance and Dispersal of Tectogenic Sediments in Thin-Skinned, Thrusted Terrains." In Frontiers in Sedimentary Geology. Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4612-3788-4_18.

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Eriksson, Kenneth A., William S. F. Kidd, and Bryan Krapez. "Basin Analysis in Regionally Metamorphosed and Deformed Early Archean Terrains: Examples from Southern Africa and Western Australia." In Frontiers in Sedimentary Geology. Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4612-3788-4_19.

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Assaad, Fakhry A., and Philip E. LaMoreaux. "Geology of Indurated Rocks, Unconsolidated Sedimentary Deposits and Karst Terrains." In Field Methods for Geologists and Hydrogeologists. Springer Berlin Heidelberg, 2004. http://dx.doi.org/10.1007/978-3-662-05438-3_2.

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Hernández-Hamón, Hernando, Paula A. Zapata-Ramírez, Rafael E. Vásquez, Carlos A. Zuluaga, Juan David Santana Mejía, and Marcela Cano. "Rapid Remote Sensing Assessment of Impacts from Hurricane Iota on the Coral Reef Geomorphic Zonation in Providencia." In Disaster Risk Reduction. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-6663-5_4.

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AbstractThis study assesses Hurricane Iota’s impact on Providencia island’s reef environments, using Google Earth Engine, Satellite Derived Bathymetry, and machine learning to calculate a supervised classification process to delineate six geomorphic reef units. Results reveal dynamic changes, including erosion in the Lagoon unit (4.47% pre-Iota, 2.27% post-Iota), loss on the Back Reef (38.14%), and Rock Terrace (6.15%). Reef Ridge showed minimal change, acting as an effective wave barrier. Back Reef and the deep Rock Terrace experienced significant erosion (−3 to −14 m) to the northeast, with

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RAVNÅS, RODMAR, KARI BERGE, HEATHER CAMPBELL, CRAIG HARVEY, and MIKE J. NORTON. "Halten Terrace Lower and Middle Jurassic inter-rift megasequence analysis." In From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin. John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118920435.ch10.

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MESSINA, CARLO, WOJCIECH NEMEC, ALLARD W. MARTINIUS, and CARSTEN ELFENBEIN. "The Garn Formation (Bajocian-Bathonian) in the Kristin Field, Halten Terrace." In From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin. John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118920435.ch18.

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Vigne, Jean‑Denis, François Briois, and Yodrik Franel. "Sector B, residential area on the slope break between the middle and lower terraces." In Klimonas. CNRS Éditions, 2024. http://dx.doi.org/10.4000/129kf.

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The excavation conducted on the slope break separating the middle from the lower terrace, less than 10 m south of the Communal building, brought to light the remains of 27 buildings cut 50–80 cm (minimum) into the slope. Fifteen of these buildings were still covered by sediment accumulations preserving their upslope circular half. This sedimentary cover was composed of thin abandonment/demolition basal layers overlain by a thick colluvial fill, accumulated after the site’s abandonment and massively reworked by Sotira excavations. The buildings were either round or elliptic, with dimensions bet

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Conference papers on the topic "Sedimentary terrain"

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Aizebeokhai, Ahzegbobor P., and Kehinde D. Oyeyemi. "Geoelectrical resistivity surveying for aquifer delineation and characterization in a sedimentary terrain, southwestern Nigeria." In SEG Technical Program Expanded Abstracts 2018. Society of Exploration Geophysicists, 2018. http://dx.doi.org/10.1190/segam2018-2990105.1.

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Abdullahi, Yusuf Mukhtar, Hafzan Eva Mansor, Mohammad Muqtada Ali Khan, et al. "Evaluation of aquifer characteristics of sedimentary terrain in Paloh area, Gua Musang, Kelantan, Malaysia." In INTERNATIONAL CONFERENCE ON BIOENGINEERING AND TECHNOLOGY (IConBET2023). AIP Publishing, 2025. https://doi.org/10.1063/5.0259310.

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Van Hove, Joel, Pete Barlow, Max Duguay, and Hamid Karimian. "Vulnerability of Pipelines Installed by Horizontal Directional Drilling to Landslides and a Proposed Framework for Developing Preliminary No Drill Zones for Landslide Avoidance." In 2022 14th International Pipeline Conference. American Society of Mechanical Engineers, 2022. http://dx.doi.org/10.1115/ipc2022-87032.

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Abstract Horizontal directional drilling (HDD) is a method of trenchless pipeline installation which has been widely used in the Western Canadian Sedimentary Basin (WCSB) during the past 40 years to cross challenging terrain, including watercourses and slopes. In the case study presented, 7,952 pipeline slope crossings are considered, of which an estimated 14% are partially or fully crossed by HDD. Often the primary objective of the HDD installation at the time of construction was to cross a watercourse and adequate consideration was not always given to the possible presence of landslide terra

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Al-Masrahy, Mohammed A., Hakima Ali Lahmar, Abdelmoniem Elaraby, and Aimen Amer. "Advanced Paleocurrent Analysis Over the Permo-Carboniferous, Methods to Reveal Its Complex Depositional History, Saudi Arabia." In International Petroleum Technology Conference. IPTC, 2024. http://dx.doi.org/10.2523/iptc-24446-ea.

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Abstract The Permo-Carboniferous deposits in Saudi Arabia display a high-level of lateral and vertical heterogeneity resulting in a complex facies architecture. Such settings can be challenging to decipher using basic techniques that depend solely on openhole logs leading to inconsistent interpretation. The aim of this paper is to examine the role of local tectonics in the formation and alternation of subsurface depositional systems and associated hydrocarbon reservoirs in the area under investigation. This is accomplished through a multidisciplinary data integration approach involving core, b

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Witte, Jan, Daniel Trümpy, Jürgen Meßner, and Hans Georg Babies. "Petroleum Potential of Rift Basins in Northern Somalia – A Fresh Look." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2573746-ms.

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ABSTRACT Several wells have encountered good oil shows in the rift basins of northern Somalia, however, without finding commercial hydrocarbons to date. It is widely accepted that these basins have a similar tectonic evolution and a comparable sedimentary fill as the highly productive rift basins in Yemen from which they have been separated by the opening of the Gulf of Aden (fully established in Mid Oligocene). We present new regional tectonic maps, new basement outcrop maps, a new structural transect and new play maps, specifically for the Odewayne, Nogal, Daroor and Socotra Basins. Digital

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Centeno-Garcia, Elena, Emiliano Campos-Madrigal, María de los Angeles Verde-Ramírez, Gilberto Silva-Romo, and Claudia Mendoza-Rosales. "CORRELATION OF JURASSIC TECTONO-SEDIMENTARY EVENTS BETWEEN AYUQUILA AND OTLALTEPEC BASINS, MIXTECA TERRANE, MEXICO." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383541.

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Wright, James, José Isola, Niall Slowey, Ronan Keating, Maya Stefanelli, and Thimothy G. Shamus. "DECIPHERING THE SEDIMENTARY RECORD ON THE PIEDRA BUENA TERRACE ALONG THE SOUTHERN ARGENTINE MARGIN." In GSA Connects 2024 Meeting in Anaheim, California. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024am-405566.

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Johnson, K. R., N. Dakin, G. D. O. Carter, and E. Phillips. "Geo-challenges for Ground Model Development in Previously Glaciated and Periglaciated Terrains." In Innovative Geotechnologies for Energy Transition. Society for Underwater Technology, 2023. http://dx.doi.org/10.3723/uclg7340.

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To achieve a net-zero clean energy future, developing offshore windfarm sites is fundamental to the UK's success in the renewable forms of energy. Integral to this is understanding the shallow subsurface geology which forms the foundation zone to these windfarm developments; particularly the impacts of past glaciations on the sedimentary and structural architecture of the deposits left behind following deglaciation. The range of depositional environments and distribution of deposits including diamictons, organic soils, rhythmically laminated soils, sands and gravels, result in extreme lateral

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Blake, David E., Justin L. Futrell, Todd A. LaMaskin, Emma R. Fishel, Lancen Tully, and David L. Barbeau. "DETRITAL ZIRCON AGES FOR METAVOLCANICLASTIC SEDIMENTARY ROCKS OF THE SPRING HOPE TERRANE, NORTH CAROLINA EASTERN PIEDMONT." In 73rd Annual GSA Southeastern Section Meeting - 2024. Geological Society of America, 2024. http://dx.doi.org/10.1130/abs/2024se-398400.

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Guan, Dayong, Geng Qian, Junpei Yue, Wenjing Pan, and Weiyan Lu. "Influence of the Tan-Lu Strike-Slip Fault Zone on Depositional Facies Distribution within the Fault Terrace Zone of the Yellow River Estuary Depression, Southern Bohai Sea, Eastern China." In International Petroleum Technology Conference. IPTC, 2025. https://doi.org/10.2523/iptc-24880-ms.

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Abstract The Bohai area is China's largest offshore crude oil production base, with proven reserves of Paleogene clastic rocks accounting for less than 30%. This positions it as a crucial production field for the future. Currently, accurately predicting the spatial distribution of these Paleogene clastic rock reservoirs remains a significant challenge. Located in the southern Bohai Sea, the fault terrace zone of the Yellow River estuary depression is bounded by the Tan-Lu strike-slip fault zone, which traverses eastern China. Recent drilling has revealed considerable variations in the spatial

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Reports on the topic "Sedimentary terrain"

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Charusiri, Punya, Wasant Pongsapich, and Chakkaphan Sutthirat. Petrochemistry of probable gem-bearing basalts in Sop Prap-Ko Kha Area, Changwat Lampang : research report. Chulalongkorn University, 1996. https://doi.org/10.58837/chula.res.1996.17.

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The project area covers approximately 300 km[superscript 2] encompassing parts of Amphoe Sop Prap, Amphoe Ko Kha, and Amphoe Mae Tha of Changwat Lampang. The area is mainly occupied by sedimentary (and metamorphic) rocks of Permian, Triassic, Tertiary and Quaternary ages. The Triassic rocks include the Phra That, the Pha Kan, and the Hong Hoi Formations of the Lampang Group. Igneous rocks comprise Permo-Triassic volcanics, Triassic granodiorite, and Cenozoic basalts. Sapphires are frequently found in alluvial and residual deposits, particularly in the northern basaltic area. Sapphires in the s

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Thompson, Anna, Michael Loso, Sydney Mooneyham, Brandon Tober, Christopher Larsen, and John Holt. Surficial geology and proglacial lake change at S?t? Tlein (Malaspina Glacier), Wrangell-St. Elias National Park and Preserve, Alaska. National Park Service, 2024. http://dx.doi.org/10.36967/2301689.

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S?t? Tlein (Tlingit for ?Big Glacier?) is the traditional name for what has recently been called Malaspina Glacier, the largest glacier in Alaska. The piedmont terminal lobe of S?t? Tlein is protected from the adjacent Pacific Ocean by a narrow, vegetated foreland dotted with proglacial lakes. Ice of the piedmont lobe is largely covered with debris and vegetation. These lakes and sedimentary deposits impact rates of melt and calving and therefore impact ongoing evolution of the glacier itself. To document these features, we present 1) a new surficial geology map for the foreland and piedmont l

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Hayward, N., and S. Paradis. Geophysical reassessment of the role of ancient lineaments on the development of the western margin of Laurentia and its sediment-hosted Zn-Pb deposits, Yukon and Northwest Territories. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/330038.

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The role of crustal lineaments in the development of the western margin of Laurentia, Selwyn basin and associated sediment-hosted Zn-Pb deposits (clastic-dominated, Mississippi-Valley-type) in Yukon and NWT, are reassessed through a new 3-D inversion strategy applied to new compilations of gravity and magnetic data. Regionally continuous, broadly NE-trending crustal lineaments including the Liard line, Fort Norman structure, and Leith Ridge fault, were interpreted as having had long-standing influence on craton, margin, and sedimentary basin development. However, multiple tectonic overprints i

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