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Relevant bibliographies by topics / Basin (Geology)

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Academic literature on the topic 'Basin (Geology)'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Basin (Geology)"

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Pronina, Natalia V., Elena Yu Makarova, Aleksandr Kh Bogomolov, Dmitriy V. Mitronov, and Evgenia V. Kuzevanova. "Geology and coal bearing capacity of the Russian Arctic in connection with prospects of development of the region." Georesursy 21, no. 2 (2019): 42–52. http://dx.doi.org/10.18599/grs.2019.2.42-52.

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Detailed geologic information can be priceless for oil- and gas- oriented geologic exploration in Arctic aquatic basins. Exploration reports on coal basins and deposits located along the Arctic coast are highly detailed and can be used for reconstruction of facies and thermobaric conditions of the poorly explored offshore areas. The article summarizes information on the Russian Arctic coal basins geology: geological structure, tectonic settings, coalforming environments and coal quality parameters. Coal basins of the region contain not only brown and bituminous coals for energetics, but include valuable coking coal (Pechorskiy, Tungusskiy, Beringovskiy basins), anthracite, thermoanthracite and graphite (Taimyrskiy, Tungusskiy basins, Dolgozhdannoye deposit), related coal methane (Pechorskiy basin, coal deposits of Spitzbergen) and trace elements (Lenskiy basin, coal basins and deposits of Chukotka and Frantz Josef Land). It is also can be used for production of advanced materials (adsorbents, sunthetic graphites, etc).

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McConachie, B. A., M. G. Barlow, J. N. Dunster, R. A. Meaney, and A. O. Schaap. "THE MOUNT ISA BASIN—DEFINITION, STRUCTURE AND PETROLEUM GEOLOGY." APPEA Journal 33, no. 1 (1993): 237. http://dx.doi.org/10.1071/aj92018.

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The Mount Isa Basin is a new concept to describe the area of Palaeo- to Mesoproterozoic rocks south of the Murphy Inlier (not the Murphy Tectonic Ridge) and inappropriately described as the Mount Isa Inlier. The new basin concept presented in this paper allows the characterisation of basin-wide structural deformation and the recognition of areas with petroleum exploration potential.The northern depositional margin of the Mount Isa Basin is the metamorphic, intrusive and volcanic complex referred to as the Murphy Inlier. The eastern, southern and western boundaries of the basin are obscured by younger basins (Carpentaria, Eromanga and Georgina Basins). The Murphy Inlier rocks comprise the seismic basement to the Mount Isa Basin sequence. Evidence for the continuity of the Mount Isa Basin with the McArthur Basin to the northwest and the Willyama Block (Basin) at Broken Hill to the south is presented. These areas combined with several other areas of similar age are believed to have comprised the Carpentarian Superbasin.The application of seismic exploration within Authority to Prospect (ATP) 423P at the northern margin of the basin was critical to the recognition and definition of the Mount Isa Basin. The northern Mount Isa Basin is structurally analogous to the Palaeozoic Arkoma Basin of Oklahoma and Arkansas in the southern USA but as with all basins it contains unique characteristics, a function of its individual development history. The northern Mount Isa Basin is defined as the basin area northwest of the Mount Gordon Fault.

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Tschirhart, Victoria, and Sally J. Pehrsson. "New insights from geophysical data on the regional structure and geometry of the southwest Thelon Basin and its basement, Northwest Territories, Canada." GEOPHYSICS 81, no. 5 (2016): B167—B178. http://dx.doi.org/10.1190/geo2015-0586.1.

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Detailed analysis of gravity and aeromagnetic data covering the southwest Thelon Basin, Northwest Territories, Canada, has provided insight into basement geology that has significance to exploration for uranium and possibly other economic metals in a remote frontier region. Interpretation of basement geology has been constrained by the calibration of gravity and magnetic signatures with Precambrian geology adjacent to the basin and sparse seismic data within the basin, creating the first basement geologic map of the southwest Thelon Basin. The basement to the overlying sedimentary units is dominated by magnetic felsic and mafic bodies variably overlying and intruding the gneissic crystalline basement. Supracrustal belts located outside the basin margins are interpreted to continue below the basin fill. Major structures have been delineated geophysically including the Howard Lake Shear Zone and the Bathurst and McDonald fault systems. Northwest-trending structures forming part of the Bathurst fault system appear to control the unconformity surface morphology and the location of basin depocenters. The geologic interpretations are corroborated by joint gravity and magnetic modeling of profiles that reveal the deepest part of the Thelon Basin reaches depths of [Formula: see text] in an area of subdued magnetic and gravimetric response to the north. The basin is a focus of active exploration for uranium, and we have found that areas along the south and eastern margins underlain by U-rich granitoid rocks may have significant potential where intersected by reactivated faults.

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Wang, Bing, Harry Doust, and Jingyan Liu. "Geology and Petroleum Systems of the East China Sea Basin." Energies 12, no. 21 (2019): 4088. http://dx.doi.org/10.3390/en12214088.

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The back-arc East China Sea Basin lies on extended continental crust at the leading edge of the Eurasian plate. In this study, the basins are described and subdivided according to their tectono-stratigraphic evolution. In order to distinguish between different phases of deformation in basin development, standard basin evolution patterns related to geodynamic drivers are identified as a first step. On the basis of this, standard patterns are recognized in the sedimentary sequences that characterize the area and its tectonic evolution, and linking them to the petroleum systems present is attempted. This is achieved by characterizing and grouping them into basin cycle-related petroleum system types (PSTs). Finally, the development of plays is examined within the petroleum systems in the context of their tectono-stratigraphic evolution, and groups of sub-basins with similar geological history and, therefore, potentially similar petroleum prospectivity are identified. In the East China Sea Basin, four proven and potential PSTs were recognized: (1) Late Cretaceous to Paleocene oil/gas-prone early syn-rift lacustrine–deltaic PST; (2) Eocene gas/oil prone late syn-rift marine PST; (3) Oligocene to Middle Miocene gas/oil-prone early post-rift fluvial–deltaic PST; (4) gas-prone syn-rift turbiditic PST. The geology and petroleum systems of three major sub-basins of the East China Sea Basin, the Xihu Sub-basin, the Lishui Sub-basin, and Okinawa Trough, are discussed in detail, and their petroleum systems and play development are analyzed. Finally, the sub-basins are grouped into “basin families” distinguished by their tectono-stratigraphic development, namely, Northwest to Northeast Shelf Basin (NWSB–NESB), Southwest to Southeast Shelf Basin (SWSB–SESB), and Okinawa Trough basin families, respectively.

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Lu, Xushan, Colin Farquharson, Jean-Marc Miehé, Grant Harrison, and Patrick Ledru. "Computer modeling of electromagnetic data for mineral exploration: Application to uranium exploration in the Athabasca Basin." Leading Edge 40, no. 2 (2021): 139a1–139a10. http://dx.doi.org/10.1190/tle40020139a1.1.

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Electromagnetic (EM) methods are important geophysical tools for mineral exploration. Forward and inverse computer modeling are commonly used to interpret EM data. Real-life geology can be complex, and our computer modeling tools need to faithfully represent subsurface features to achieve accurate data interpretation. Traditional rectilinear meshes are less flexible and have difficulty conforming to the complex geometries of realistic geologic models, resulting in large numbers of mesh cells. In contrast, unstructured grids can represent complex geologic structures efficiently and accurately. However, building realistic geologic models and discretizing these models with unstructured grids suitable for EM modeling can be difficult and requires significant effort and specialized computer software tools. Therefore, it is important to develop workflows that can be used to facilitate model building and mesh generation. We have developed a procedure that can be used to build arbitrarily complex geologic models with topography using unstructured grids and a finite-volume time-domain code to calculate EM responses. We present an example of a trial-and-error modeling approach applied to a real data set collected at a uranium exploration project in the Athabasca Basin in Canada. The uranium mineralization is closely related to graphitic fault conductors in the basement. The deep burial depth and small thickness of the graphitic fault conductors demand accurate data interpretation results to guide subsequent drill testing. Our trial-and-error modeling approach builds initial realistic geologic models based on known geology and downhole data and creates initial geoelectrical models based on physical property measurements. Then, the initial model is iteratively refined based on the match between modeled and real data. We show that the modeling method can obtain 3D geoelectrical models that conform to known geology while achieving a good match between modeled and real data. The method can also provide guidance of where future drill holes should be directed.

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BOGDANOV, Nikita A. "GEOLOGY OF THE KOMANDORSKY DEEP BASIN." Journal of Physics of the Earth 36, Proceeding1 (1988): S65—S71. http://dx.doi.org/10.4294/jpe1952.36.proceeding1_s65.

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BIEN, M. N. "Geology of the Yuanmo Basin, Yunnan*." Bulletin of the Geological Society of China 20, no. 1 (2009): 23–32. http://dx.doi.org/10.1111/j.1755-6724.1940.mp20001003.x.

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Caplan, Charlotte A., Helen C. Gildersleeves, Al G. Harding, et al. "Geology of the Northwestern Krania Basin." Bulletin of the Geological Society of Greece 54, no. 1 (2019): 113. http://dx.doi.org/10.12681/bgsg.19375.

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We present a new map of 30 km2 of the northwestern Krania Basin at 1:10,000 scale, including rocks of the Pindos Ophiolite Group and associated units, and the sedimentary fill of the Krania Basin. The Krania Basin is a flexural basin developed in the Middle – Late Eocene and filled first with alluvial fan conglomerates and later with turbidite sandstones and siltstones, following a deepening of the basin. Analysis of the clasts within the sediment, combined with paleoflow analyses, suggest sediment input from the eroding Pindos Ophiolite to the west. The Pindos Ophiolite Group is represented in the area by pillow lavas, sheeted dykes and serpentinized harzburgites of the Aspropotamos Complex. The ophiolite forms imbricated, thrust bounded blocks which show two phases of thrusting, corresponding to Late Jurassic and Eocene stages of ophiolite emplacement. We identify five stages of deformation within the basin itself, starting with Early - Middle Eocene syndepositional extensional faulting associated with the formation of the basin. This was followed by four stages of post-depositional deformation, starting with Late Eocene compression associated with basin closure, which caused thrust faulting and folding of the sediments. Oligocene dextral faulting with a thrust component affected the basin margins. Finally, two normal faulting events with different orientations have affected the basin since the Miocene.

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Richards, P. C., and N. G. T. Fannin. "GEOLOGY OF THE NORTH FALKLAND BASIN." Journal of Petroleum Geology 20, no. 2 (1997): 165–83. http://dx.doi.org/10.1111/j.1747-5457.1997.tb00771.x.

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Lirong, Dou, Cheng Dingsheng, Li Zhi, Zhang Zhiwei, and Wang Jingchun. "PETROLEUM GEOLOGY OF THE FULA SUB-BASIN, MUGLAD BASIN, SUDAN." Journal of Petroleum Geology 36, no. 1 (2012): 43–59. http://dx.doi.org/10.1111/jpg.12541.

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Dissertations / Theses on the topic "Basin (Geology)"

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Zahid, Khandaker Uddin Ashraf. "Provenance and basin tectonics of Oligocene-Miocene sequences of the Bengal Basin, Bangladesh." Auburn, Ala., 2005. http://repo.lib.auburn.edu/2005%20Fall/Thesis/ZAHID_KHANDAKER_14.pdf.

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Aspler, Lawrence B. (Lawrence Bernard) Carleton University Dissertation Geology. "Geology of Nonacho Basin (early Proterozoic) N.W.T." Ottawa, 1985.

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Hawkes, Martin. "Surficial geology of the Boston basin, Ma." Thesis, Massachusetts Institute of Technology, 1987. http://hdl.handle.net/1721.1/14816.

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Bauer, Tobias. "Structural and sedimentological reconstruction of the inverted Vargfors basin : a base for 4D-modelling." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-17596.

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The Palaeoproterozoic Skellefte mining district in northern Sweden covers an area of 120 by 30 km and is one of the most important mining districts in Europe, producing mainly Zn, Cu, Pb, As and Au from volcanogenic massive sulfide (VMS) and orogenic gold deposits.Detailed mapping of structures and stratigraphy within the sedimentary Vargfors Group combined with a structural analysis revealed a syn-extensional fault pattern of NW-SE-trending normal faults and associated NE-SW-trending transfer faults, creating the segmented sedimentary Vargfors basin. It comprises distinct fault-bound compartments, which incluence the sedimentary stratigraphy in each of these compartments.Syn-rift subsidence affected the sedimentary conditions from near-shore to shallow submarine environment.Intensive fault movements associated with mafic volcanic activity along these faults resulted in the rapid uplift of the oldest phase of the Jörn intrusive complex and/or subsidence of its surrounding areas. Subsequent erosion of the intrusive rocks led to the formation of a tonalite to granodiorite bearing conglomeratic sequence, representing an alluvial fan. Further uplift to the north of the district resulted in the erosion of Arvidsjaur volcanic rocks and the formation of a braided river system. Subsidence of the intrusive complex and/or a sedimentary coverage on top of the same caused a break in sedimentation of tonalite to granodiorite clasts. Stratigraphical evolution of the sedimentary rocks and the Vargfors Group - Skellefte Group contact relationships show that rifting started in the centre and proceeded with time towards SE and NW. Subsequent basin inversion resulted in the reactivation of the existing normal faults along a carbonate-rich basal layer forming asymmetric synclines. Primary geometries of sedimentary strata within each fault-bound compartment controlled their deformation styles. Furthermore, strain was partitioned into the faults, forming high strain zones along the basin margins, where foliations parallel the main faults, and low strain domains in the core of the basin, where foliation is oblique to the main structural grain of the basin. This oblique foliation is either a result of a rotating stress field or a transpressional regime. This case study on basin inversion gives implications for accretion processes along the Svecokarelian Craton margin as well as forthe formation of VMS-deposits and their possible transposition. Basic modelling of the main geological boundaries in the central Skellefte district was performed by integrating data from regional to outcrop scale using the GoCAD (Paradigm) software platform. Available data included geographical and geological data, which were imported from ArcGIS (ESRI) as well as drill-hole data, seismic profiles, resistivity and gravimetry profiles and EM-profiles. Creation of the main geological boundaries utilized GoCAD and SPARSE (Mirageoscience) algorithms, whereas structural geological data was exclusively modelled with SPARSE. Furthermore, this study provides a base for refining the 3-dimensional model and developing a 4-dimensional model, showing the geological evolution of the Skellefte district.<br>Godkänd; 2010; 20101029 (tobbau); LICENTIATSEMINARIUM Ämnesområde: Malmgeologi/Ore Geology Examinator: Professor Pär Weihed, Luleå tekniska universitet Diskutant: Dr Peter Sorjonen-Ward, GTK, Kuopio, Finland Tid: Torsdag den 16 december 2010 kl 10.00 Plats: F531, Luleå tekniska universitet

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Mohamed, Abdalla Yagoub. "Basin analysis and hydrocarbon maturation, Unity and Kaikang area, Muglad Basin, Sudan." Thesis, University of Aberdeen, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.390934.

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Basin analysis study has been conducted along a cross section in the Unity-Kaikang area, Muglad Basin, Sudan. The research is based essentially on geological, seismic investigations and basin model approach. The basin model approach included two dimensional gravity modelling, and one dimensional thermal history, maturation and hydrocarbon generation modelling. In addition an investigation of the hydrocarbon migration processes, routes to the known and probable accumulation targets is studied. The basin models were calibrated against data obtained from wells drilled in the area. The seismic investigations indicate a sedimentary thickness ranging from 11 to 7 km averaging 9 km along the area of the cross section. The two dimensional gravity model suggests a mantle uplift of 2.18 km and a β stretching factor of 1.47 with a thin crust of 24 km, corresponding to an extension of 45 km. The burial and thermal model suggests a high subsidence rate accompanied by a slow sedimentation rate during the Neocomian and Aptian times. The present heat flow is ranging between 72 (Kaikang area) to 50 mW/m<sup>2</sup> averaging 59 mW/m<sup>2</sup> along the cross section of the study area. The paleoheat flow is averaging 57 mW/m<sup>2</sup> with peaks of 65 mW/m<sup>2</sup> during the Aptian-Senomanian, Paleocene to Eocene times and a last peak of 59 mW/m<sup>2</sup> between the Miocene and the present. The maturation and hydrocarbon generation model (LLNL, Sweeny 1990) has been applied to the oil prone source rocks of the Abu Gabra and Sharaf formations. For the purpose of modelling the Abu Gabra Formation has been divided into three layers. In the top layers of the Abu Gabra Formation, the model predicts an average onset of oil generation at 90 Ma and an end at 10 Ma. In the combined source rock section of layer three of the Abu Gabra and the Sharaf Formation the model predicts an average onset of oil generation at 110 and an end at 30 Ma.

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Cloke, Ian Richard. "Structural controls on basin evolution in the Kutai Basin and Mekassar Straits." Thesis, Royal Holloway, University of London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.285157.

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The Kutai basin is an inverted extensional basin located onshore Borneo, to the west of the Makassar Straits. Basin initiation had occurred by the middle Eocene and was contemporaneous with oblique oceanic spreading in the Makassar Straits. Field studies, geophysical data and computer modelling elucidate the structural evolution of the rift basin. Vein sets, C-S fabrics and chevron folds were studied in the lurassicCretaceous basement and NW-SE and NE-SW trending fractures were reactivated during the Tertiary controlling the basin architecture. Seismic profiles across both the northern and southern margins of the Kutai Basin show inverted middle Eocene halfgraben. These were infilled by syn-rift successions that demonstrate considerable lateral and vertical facies variations. Provenance studies of syn-rift sediments suggest differing source areas for individual half-graben. Offsets of middle Eocene carbonate horizons and thickening of syn-tectonic units seen on seismic sections, indicate late Oligocene extension on NW-SE trending en-echelon extensional faults. Middle Miocene inversion was concentrated on east-facing half-graben and asymmetric inversion anticlines are found on both the northern and southern margins of the Kutai basin. Structural data from these anticlines suggest a shortening direction oriented 290°-310°. The presence of dominantly WNW vergent thrusts indicates compression from the ESE. During the middle Eocene graben-bounding faults initially formed offset enechelon arrays trending N-S, NNE-SSW and NE-SW characteristic of oblique extension of a basement fabric. Reactivation of these structures led to breaching of relay ramps and 'hard-linkage' of faults. The orientation of middle Eocene dykes and faults show the extension direction was oriented WNW-ESE. A reorientation of the stress direction during the late Oligocene was inferred from extension on en-echelon NW-SE trending faults. A rotation of the extension direction by between 45 and 60° counter-clockwise is suggested by fault and vein orientations. Neogene micro-continental collisions with the margins of northern and eastern Sundaland strongly influenced the inversion of the basin. Inversion was focused in the weak attenuated crust underlying the Kutai basin and adjacent basins, whereas the stronger oceanic crust underlying the northern Makassar Straits acted as a passive conduit for compressional stresses. This study has implications for the development of rift basins associated with oceanic spreading and for regional tectonics.

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Huson, Sarah Ann. "Structural study of the southwest part of Elk Basin Anticline, Bighorn Basin, Wyoming." Virtual Press, 2002. http://liblink.bsu.edu/uhtbin/catkey/1236575.

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A subsurface and surface structural study was completed in the southwest part of the Elk Basin Anticline, Wyoming. The goals of this study were to better improve preexisting geologic surface maps of the area and to better understand subsurface structural relationships. A normal fault with a splay to the north was recorded through sections 25, 26. and 35 of T58N, RI00W. Using well logs to create across section, this fault was traced in the subsurface. Strike and dip measurements in undisturbed areas of the anticline averaged 332° (azimuth) or N28W (quadrant). In an area of anomalous strike (section 26 of T58N, R1 00W), strike readings averaged 303° (azimuth) or N57W (quadrant). This region has been interpreted as an area rotated counter clockwise due to drag on a subsurface tear fault located at the northern end of the anticline. The current study is significant since it lends support to a little studied Laramide structural feature.<br>Department of Geology

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Mohapatra, Gopal Krishna 1968. "Faulting and basin geometry beneath the Great Salt Lake: implications for basin evolution and cenozoic extension." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/565551.

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Hamlin, Herbert Scott. "Syn-orogenic slope and basin depositional systems, Ozona sandstone, Val Verde Basin, southwest Texas /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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Fothergill, Patrick Allen. "Late Tertiary and Quaternary intermontane basin evolution in north-east Tibet : the Guide Basin." Thesis, Royal Holloway, University of London, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.299105.

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Books on the topic "Basin (Geology)"

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Geology of the Great Basin. University of Nevada Press, 1986.

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Gupta, A. B. Das. Geology of N.W. Bengal Basin. Geological Society of India, 2006.

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Fiero, Bill. Geology of the Great Basin. University of Nevada Press, 1986.

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McPhee, John. Basin and range. Noonday Press, 1990.

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Shannon, P. Petroleum basin studies. Graham & Trotman, 1989.

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Olsen, Henrik. Sedimentary basin analysis of the continental Devonian basin in North-East Greenland. Grønlands geologiske undersøgelse, 1993.

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Tian, Zaiyi. Petroliferous sedimentary basins in China and basin analysis. Petroleum Industry Press, 1997.

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Lerche, I. Basin analysis: Quantitative methods. Academic Press, 1990.

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Ozimic, S. Gippsland Basin, Victoria. Australian Government Pub. Service, 1987.

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1942-, Moors H. T., Ghori K. A. R, and Geological Survey of Western Australia., eds. Basin development and petroleum exploration potential of the Yowalga Area, Officer Basin, Western Australia. Geological Survey of Western Australia, 2000.

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Book chapters on the topic "Basin (Geology)"

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Jiang, Zaixing. "The Emergence of Windfield-Source-Basin Dynamics." In Springer Geology. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-7407-3_1.

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Jiang, Zaixing. "Depositional Systems and Windfield-Source-Basin System Dynamics of the West Sag, Liaohe Depression, Bohai Bay Basin." In Springer Geology. Springer Singapore, 2018. http://dx.doi.org/10.1007/978-981-10-7407-3_5.

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Holz, Michael, Edric Troccoli, and Marcelo Vieira. "Sequence Stratigraphy of Continental Rift Basins II: An Example from the Brazilian Cretaceous Recôncavo Basin." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_3.

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Bjørlykke, Knut Olav. "Seismic Stratigraphy and Basin Analysis." In Sedimentology and Petroleum Geology. Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-72592-0_11.

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Haas, János, András Nagymarosy, and Géza Hámor. "Genesis and Evolution of the Pannonian Basin." In Geology of Hungary. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-21910-8_3.

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Frimmel, Hartwig E. "The Witwatersrand Basin and Its Gold Deposits." In Regional Geology Reviews. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-78652-0_10.

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Hawkins, James W. "The Geology of the Lau Basin." In Backarc Basins. Springer US, 1995. http://dx.doi.org/10.1007/978-1-4615-1843-3_3.

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Tedford, Richard H., Zhan-Xiang Qiu, and Jie Ye. "Cenozoic Geology of the Yushe Basin." In Late Cenozoic Yushe Basin, Shanxi Province, China: Geology and Fossil Mammals. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-90-481-8714-0_3.

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Lukševičs, Ervīns, Ģirts Stinkulis, Tomas Saks, Konrāds Popovs, and Jānis Jātnieks. "The Devonian Stratigraphic Succession and Evolution of the Baltic Sedimentary Basin." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_103.

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Paris, F., and G. Le Pochat. "The Aquitaine Basin." In Pre-Mesozoic Geology in France and Related Areas. Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-84915-2_31.

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Conference papers on the topic "Basin (Geology)"

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Kozlowski, E. "Structural Geology of the NW Neuquina Basin." In 4th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 1991. http://dx.doi.org/10.3997/2214-4609-pdb.115.001eng.

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H. Bachmann, G., and M. Muller. "Petroleum geology of the German Molasse Basin." In 56th EAEG Meeting. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609.201410138.

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Greb, Stephen F., and Cortland F. Eble. "ILLINOIS BASIN COAL RESOURCES AND MINING GEOLOGY." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323578.

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Gammudi, A. "Palaeoenvironments of the Palaeogene in the Sirt Basin." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201405990.

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Crigo, D., C. Daturi, and C. Rizzi. "Tunisia Offshore a Basin Modelling Assisted Exploration History." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406032.

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Y. Ali, M. "Petroleum Geology and Hydrocarbon Potential of Guban Basin (Bihendula Basin), Somaliland." In 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201401660.

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Grabowski, G. J. "Stratigraphy and Depositional History of the Marib-Jawf Basin, Yemen." In Fourth Arabian Plate Geology Workshop. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142784.

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Leite, J., T. W. Schirmer, and B. R. Laws. "Lower Congo Basin, Deepwater Exploration Province, Offshore West Africa." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406024.

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Rapti, B., U. Erkmen, A. Hadia, R. Gardner, and D. Neilson. "A Multidisciplinary Evaluation of Producing Satal Carbonates Sirt Basin, Libya." In EAGE Conference on Geology and Petroleum Geology of the Mediterranean and Circum-Mediterranean Basins. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609.201406033.

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Barredo, Silvia Patricia, and Luis Pedro Stinco. "Unconventional Reservoir Geology of the Neuquén Basin Argentina." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 2014. http://dx.doi.org/10.2118/170905-ms.

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Reports on the topic "Basin (Geology)"

1

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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Gordey, S. P. Geology, Selwyn Basin (105J and 105K), Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225395.

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3

Campbell, J. E. Quaternary geology of the eastern Athabasca Basin, Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2007. http://dx.doi.org/10.4095/223764.

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4

Owens, R. J., I. Borissova, L. S. Hall, et al. Geology and prospectivity of the northern Houtman Sub-basin. Geoscience Australia, 2018. http://dx.doi.org/10.11636/record.2018.025.

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Merritt, R. D. Coal geology and resources of the Nenana Basin, Alaska. Alaska Division of Geological & Geophysical Surveys, 1986. http://dx.doi.org/10.14509/1264.

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Ryan, R. J. Geology of the Tatamagouche Syncline, Cumberland Basin, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130049.

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7

Gordey, S. P. Geology, Selwyn Basin (Sheldon Lake and Tay River), Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/288980.

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8

Higgs, R. Sedimentology, Basin - Fill Architecture and Petroleum Geology of the Teritary Queen Charlotte Basin, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131979.

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9

Forbes, D. L., K. Moran, J. Zevenhuizen, and J. Shaw. Surficial geology and physical properties 12: central shelf: Emerald Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210707.

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Moran, K., J. Zevenhuizen, and I. Kulin. Surficial geology and physical properties 13: central shelf: basin comparison. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/210708.

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