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Relevant bibliographies by topics / Orthogonal rift basin

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Academic literature on the topic 'Orthogonal rift basin'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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Journal articles on the topic "Orthogonal rift basin"

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Milia, Alfonsa, and Maurizio M. Torrente. "Extensional Messinian basins in the Central Mediterranean (Calabria, Italy): new stratigraphic and tectonic insights." Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 73 (2018): 45. http://dx.doi.org/10.2516/ogst/2018040.

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The direction of extension and the architecture of the Messinian basins of the Central Mediterranean region is a controversial issue. By combining original stratigraphic analysis of wells and seismic profiles collected offshore and onshore Calabria, we reassess the tectonic evolution that controlled the sedimentation and basement deformation during Messinian times. Three main deep sedimentary basins in the Calabria area record a Messinian succession formed by two clays/shales-dominated subunits subdivided by a halite-dominated subunit. The correlation with the worldwide recognized stratigraphi

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Mortimer, E., D. A. Paton, C. A. Scholz, M. R. Strecker, and P. Blisniuk. "Orthogonal to oblique rifting: effect of rift basin orientation in the evolution of the North basin, Malawi Rift, East Africa." Basin Research 19, no. 3 (2007): 393–407. http://dx.doi.org/10.1111/j.1365-2117.2007.00332.x.

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O'Brien, G. W., M. A. Etheridge, J. B. Willcox, et al. "THE STRUCTURAL ARCHITECTURE OF THE TIMOR SEA, NORTH-WESTERN AUSTRALIA: IMPLICATIONS FOR BASIN DEVELOPMENT AND HYDROCARBON EXPLORATION." APPEA Journal 33, no. 1 (1993): 258. http://dx.doi.org/10.1071/aj92019.

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The initial rifting in the Timor Sea, north-western Australia, took place in the Late Devonian to Early Carboniferous, with the development of the NWtrending Petrel Sub-basin. This rift system was compartmentalised by NE-trending accommodation zones which divided the sub-basin into discrete segments. In each segment, a lower plate rift margin, characterised by large displacement, low angle extensional faults, lay opposite an upper plate, or ramp, rift margin, characterised by small displacement, high angle flexural faults. Switching in the 'polarity' of the rift system took place across major,

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Stacey, Andrew, Cameron Mitchell, Goutam Nayak, et al. "Geology and petroleum prospectivity of the deepwater Otway and Sorell basins: new insights from an integrated regional study." APPEA Journal 51, no. 2 (2011): 692. http://dx.doi.org/10.1071/aj10072.

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The frontier deepwater Otway and Sorell basins lie offshore of southwestern Victoria and western Tasmania at the eastern end of Australia’s Southern Rift System. The basins developed during rifting and continental separation between Australia and Antarctica from the Cretaceous to Cenozoic. The complex structural and depositional history of the basins reflects their location in the transition from an orthogonal–obliquely rifted continental margin (western–central Otway Basin) to a transform continental margin (southern Sorell Basin). Despite good 2D seismic data coverage, these basins remain re

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Lagabrielle, Yves, Riccardo Asti, Serge Fourcade, et al. "Mantle exhumation at magma-poor passive continental margins. Part I. 3D architecture and metasomatic evolution of a fossil exhumed mantle domain (Urdach lherzolite, north-western Pyrenees, France)." BSGF - Earth Sciences Bulletin 190 (2019): 8. http://dx.doi.org/10.1051/bsgf/2019007.

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In two companion papers, we report the detailed geological and mineralogical study of two emblematic serpentinized ultramafic bodies of the western North Pyrenean Zone (NPZ), the Urdach massif (this paper) and the Saraillé massif (paper 2). The peridotites have been exhumed to lower crustal levels during the Cretaceous rifting period in the future NPZ. They are associated with Mesozoic pre-rift metamorphic sediments and small units of thinned Paleozoic basement that were deformed during the mantle exhumation event. Based on detailed geological cross-sections and microprobe mineralogical analys

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Anfiloff, V. "The effect of vertical crustal fractures on the rifting process." Exploration Geophysics 20, no. 2 (1989): 175. http://dx.doi.org/10.1071/eg989175.

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In the past, rifts have mainly been identified in terms of sediment troughs. They account for many of the elongate gravity lows distributed in a coherent rectilinear manner over the continent. Other gravity lows can be attributed to granites intruding rift compartments, and some gravity highs can be attributed to basic volcanics in compartments. The total number of rifts which can be thus inferred from gravity and magnetics is very large, and suggests rifting is pervasive over the whole continent and controlled by a systematically distributed "Cardinal" system of ancient vertical crustal fract

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Guiraud, M., A. Buta-Neto, and D. Quesne. "Segmentation and differential post-rift uplift at the Angola margin as recorded by the transform-rifted Benguela and oblique-to-orthogonal-rifted Kwanza basins." Marine and Petroleum Geology 27, no. 5 (2010): 1040–68. http://dx.doi.org/10.1016/j.marpetgeo.2010.01.017.

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Bartaschuk, Оleksii, and Vasyl Suyarko. "GEODYNAMICS." GEODYNAMICS 1(30)2021, no. 1(30) (2021): 25–35. http://dx.doi.org/10.23939/jgd2021.01.025.

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The second part of the article studies the tectonic conditions and natural mechanisms of tectonic inversion of the Dnieper-Donets Basin and the Western Donets Graben. Method. The research uses the original method of reconstruction of fields of tectonic stresses and deformations. It also makes tectonophysical analysis of geostructures was used. The analytical base of the research consisted of the latest materials of geo-mapping, numerical modeling of deformations of the southern edge of the Eastern European platform and comparison of model and reconstructed stress fields. Results. In the geodyn

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Hoffman, P. F. "On the kinematics and timing of Rodinia breakup: a possible rift–transform junction of Cryogenian age at the southwest cape of Congo Craton (northwest Namibia)." South African Journal of Geology, May 31, 2021. http://dx.doi.org/10.25131/sajg.124.0038.

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Abstract After tilt correction for Ediacaran thick-skinned folding, a pair of Cryogenian half grabens at the autochthonous southwest cape of Congo Craton (CC) in northwest Namibia restore to different orientations. Toekoms sub-basin trended east-northeast, parallel to Northern Zone (NZ) of Damara belt, and was bounded by a normal-sense growth fault (2 290 m throw) dipping 57° toward CC. Soutput sub-basin trended northwest, oblique to NZ and to north-northwest-trending Kaoko Belt. It was bounded by a growth fault (750 m down-dip throw) dipping steeply (~75°) toward CC. Soutput growth fault coul

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Dissertations / Theses on the topic "Orthogonal rift basin"

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Blanco, Andr? Jo?o Palma Conde. "Modelagem estrutural f?sica de semigr?ben ortogonais e obl?quos ? disten??o regional: influ?ncia da trama do embasamento e compara??o com anal?gicos no nordeste brasileiro." Universidade Federal do Rio Grande do Norte, 2013. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18834.

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Made available in DSpace on 2015-03-13T17:08:37Z (GMT). No. of bitstreams: 1 AndreJPCB_DISSERT.pdf: 4384821 bytes, checksum: f23022c7fe9a0e10cf6b38d62f412fc4 (MD5) Previous issue date: 2013-06-17<br>The physical structural modeling tool is being increasingly used in geology to provide information about the evolutionary stages (nucleation, growth) and geometry of geological structures at various scales. During the simulations of extensional tectonics, modeling provides a better understanding of fault geometry and evolution of the tectonic-stratigraphic architecture of rift basins. In this s

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