Relevant bibliographies by topics / Foreland basins

Contents

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

Academic literature on the topic 'Foreland basins'

Author: Grafiati
Published: 4 June 2021
Last updated: 2 February 2022

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Foreland basins.'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Foreland basins"

1

Thomas, William A., George E. Gehrels, Kurt E. Sundell, and Mariah C. Romero. "Detrital-zircon analyses, provenance, and late Paleozoic sediment dispersal in the context of tectonic evolution of the Ouachita orogen." Geosphere 17, no. 4 (May 14, 2020): 1214–47. http://dx.doi.org/10.1130/ges02288.1.

Full text
Abstract:
Abstract New analyses for U-Pb ages and εHft values, along with previously published U-Pb ages, from Mississippian–Permian sandstones in synorogenic clastic wedges of the Ouachita foreland and nearby intracratonic basins support new interpretations of provenance and sediment dispersal along the southern Midcontinent of North America. Recently published U-Pb and Hf data from the Marathon foreland confirm a provenance in the accreted Coahuila terrane, which has distinctive Amazonia/Gondwana characteristics. Data from Pennsylvanian–Permian sandstones in the Fort Worth basin, along the southern arm of the Ouachita thrust belt, are nearly identical to those from the Marathon foreland, strongly indicating the same or a similar provenance. The accreted Sabine terrane, which is documented by geophysical data, is in close proximity to the Coahuila terrane, suggesting the two are parts of an originally larger Gondwanan terrane. The available data suggest that the Sabine terrane is a Gondwanan terrane that was the provenance of the detritus in the Fort Worth basin. Detrital-zircon data from Permian sandstones in the intracratonic Anadarko basin are very similar to those from the Fort Worth basin and Marathon foreland, indicating sediment dispersal from the Coahuila and/or Sabine terranes within the Ouachita orogen cratonward from the immediate forelands onto the southern craton. Similar, previously published data from the Permian basin suggest widespread distribution from the Ouachita orogen. In contrast to the other basins along the Ouachita-Marathon foreland, the Mississippian–Pennsylvanian sandstones in the Arkoma basin contain a more diverse distribution of detrital-zircon ages, indicating mixed dispersal pathways of sediment from multiple provenances. Some of the Arkoma sandstones have U-Pb age distributions like those of the Fort Worth and Marathon forelands. In contrast, other sandstones, especially those with paleocurrent and paleogeographic indicators of southward progradation of depositional systems onto the northern distal shelf of the Arkoma basin, have U-Pb age distributions and εHft values like those of the “Appalachian signature.” The combined data suggest a mixture of detritus from the proximal Sabine terrane/Ouachita orogenic belt with detritus routed through the Appalachian basin via the southern Illinois basin to the distal Arkoma basin. The Arkoma basin evidently marks the southwestern extent of Appalachian-derived detritus along the Ouachita-Marathon foreland and the transition southwestward to overfilled basins that spread detritus onto the southern craton from the Ouachita-Marathon orogen, including accreted Gondwanan terranes.
APA, Harvard, Vancouver, ISO, and other styles
2

Zhang, Hong. "Accumulation Models of the Natural Gas in the Foreland Basins of China and their Physical Simulation Experiment." Advanced Materials Research 233-235 (May 2011): 2812–15. http://dx.doi.org/10.4028/www.scientific.net/amr.233-235.2812.

Full text
Abstract:
The paper chooses foreland basin as its research object. after summarizing the accumulation characteristics of the different phases and different parts of them, the common models of the whole foreland basin are given and the physical simulation experiments are carried out. It shows that the foreland basins experience three phases of evolution. Phase 1 is the period that the source rock and structure oil and gas traps form. Phase 2 is the period that multi-cycle reservoir and lithologic oil and gas pool form. phase 3 is the period that foreland uplift belt and fault anticline pool form. Then a foreland basins has three different belts including of thrust belt, foredeep and foreland slope belt, foreland uplift belt, and the belts have different accumulation models. With regard to the hydrocarbon accumulation period of the foreland basin, the thrust belt have precedence to other belt. foredeep and foreland slope belt forms the secondary pools. Foreland uplift belt accumulates hydrocarbon very quickly.
APA, Harvard, Vancouver, ISO, and other styles
3

Tankard, Anthony. "Cenozoic Foreland Basins of Europe." Sedimentary Geology 152, no. 1-2 (September 2002): 160–61. http://dx.doi.org/10.1016/s0037-0738(01)00257-3.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Naylor, M., and H. D. Sinclair. "Pro- vs. retro-foreland basins." Basin Research 20, no. 3 (April 24, 2008): 285–303. http://dx.doi.org/10.1111/j.1365-2117.2008.00366.x.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Roberts, G. P. "Foreland basins and fold belts." Journal of Structural Geology 16, no. 1 (January 1994): 143–44. http://dx.doi.org/10.1016/0191-8141(94)90025-6.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Daly, M. C. "Foreland basins and fold belts." Marine and Petroleum Geology 11, no. 4 (August 1994): 507–8. http://dx.doi.org/10.1016/0264-8172(94)90085-x.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Lawton, Timothy F., Jeffrey M. Amato, Sarah E. K. Machin, John C. Gilbert, and Spencer G. Lucas. "Transition from Late Jurassic rifting to middle Cretaceous dynamic foreland, southwestern U.S. and northwestern Mexico." GSA Bulletin 132, no. 11-12 (April 8, 2020): 2489–516. http://dx.doi.org/10.1130/b35433.1.

Full text
Abstract:
Abstract Subsidence history and sandstone provenance of the Bisbee basin of southwestern New Mexico, southern Arizona, and northern Sonora, Mexico, demonstrate basin evolution from an array of Late Jurassic–Early Cretaceous rift basins to a partitioned middle Cretaceous retroarc foreland basin. The foreland basin contained persistent depocenters that were inherited from the rift basin array and determined patterns of Albian–early Cenomanian sediment routing. Upper Jurassic and Valanginian–Aptian strata were deposited in three narrow extensional basins, termed the Altar-Cucurpe, Huachuca, and Bootheel basins. Initially rapid Late Jurassic subsidence in the basins slowed in the Early Cretaceous, then increased again from mid-Albian through middle Cenomanian time, marking an episode of foreland subsidence. Sandstone composition and detrital zircon provenance indicate different sediment sources in the three basins and demonstrate their continued persistence as depocenters during Albian foreland basin development. Late Jurassic basins received sediment from a nearby magmatic arc that migrated westward with time. Following a 10–15 m.y. depositional hiatus, an Early Cretaceous continental margin arc supplied sediment to the Altar-Cucurpe basin in Sonora as early as ca. 136 Ma, but local sedimentary and basement sources dominated the Huachuca basin of southern Arizona until catchment extension tapped the arc source at ca. 123 Ma. The Bootheel basin of southwestern New Mexico received sediment only from local basement and recycled sedimentary sources with no contemporary arc source evident. During renewed Albian–Cenomanian subsidence, the arc continued to supply volcanic-lithic sand to the Altar-Cucurpe basin, which by then was the foredeep of the foreland basin. Sandstone of the Bootheel basin is more quartzose than the Altar-Cucurpe basin, but uncommon sandstone beds contain neovolcanic lithic fragments and young zircon grains that were transported to the basin as airborne ash. Latest Albian–early Cenomanian U-Pb tuff ages, detrital zircon maximum depositional ages ranging from ca. 102 Ma to 98 Ma, and ammonite fossils all demonstrate equivalence of middle Cretaceous proximal foreland strata of the U.S.-Mexico border region with distal back-bulge strata of the Cordilleran foreland basin. Marine strata buried a former rift shoulder in southwestern New Mexico during late Albian to earliest Cenomanian time (ca. 105–100 Ma), prior to widespread transgression in central New Mexico (ca. 98 Ma). Lateral stratigraphic continuity across the former rift shoulder likely resulted from regional dynamic subsidence following late Albian collision of the Guerrero composite volcanic terrane with Mexico and emplacement of the Farallon slab beneath the U.S.–Mexico border region. Inferred dynamic subsidence in the foreland of southern Arizona and southwestern New Mexico was likely augmented in Sonora by flexural subsidence adjacent to an incipient thrust load driven by collision of the Guerrero superterrane.
APA, Harvard, Vancouver, ISO, and other styles
8

Roberts, D. G. "Cenozoic Foreland Basins of Western Europe." Marine and Petroleum Geology 18, no. 3 (March 2001): 441. http://dx.doi.org/10.1016/s0264-8172(00)00063-5.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

González-Bonorino, G., P. Kraemer, and G. Re. "Andean Cenozoic foreland basins: a review." Journal of South American Earth Sciences 14, no. 7 (December 2001): 651–54. http://dx.doi.org/10.1016/s0895-9811(01)00073-6.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Vezzoli, Giovanni, and Eduardo Garzanti. "Tracking Paleodrainage in Pleistocene Foreland Basins." Journal of Geology 117, no. 4 (July 2009): 445–54. http://dx.doi.org/10.1086/598946.

Full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Dissertations / Theses on the topic "Foreland basins"

1

Bry, Madeleine. "Flexure of the lithosphere at foreland basins." Thesis, University of Cambridge, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.439115.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Booth, Sophie Catherine. "Causes of subsidence within retroarc foreland basins." Thesis, University of Liverpool, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367069.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Edwards, Christopher Mark. "The evolution of accommodation in retroarc foreland basins." Thesis, University of Liverpool, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.402683.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Luo, Hongjun. "Tectonostratigraphy of foreland basins the Upper Cretaceous in southwestern Wyoming /." Laramie, Wyo. : University of Wyoming, 2005. http://proquest.umi.com/pqdweb?did=990280521&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Cole, John E. "The comparative tectonic evolution of variscan coal-bearing foreland basins." Thesis, Cardiff University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.360572.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Sinclair, Hugh D. "The North Helvetic Flysch of eastern Switzerland : Foreland Basin architecture and modelling." Thesis, University of Oxford, 1989. http://ora.ox.ac.uk/objects/uuid:0e83a6d2-cf51-4dd3-b4bb-523a1d28fc90.

Full text
Abstract:
The North Alpine Foreland Basin (NAFB) comprises sediments of late Eocene to middle Miocene age. The earliest deposits are the North Helvetic Flysch which are exposed in the regions of Glarus and Graubunden, eastern Switzerland. The Taveyannaz sandstones are the first thrust wedge (southerly) derived sediments of the North Helvetic Flysch. The Taveyannaz basin was divided into two sub-basins by a thrust ramp palaeohigh running ENE/WSW (parallel to the thrust front). Palaeocurrent directions were trench parallel towards the ENE. Sedimentation in the Inner basin (140m thick) is characterised by very thick bedded turbidite sands generated by thrust induced seismic events confined within the thrust-top basin. The Outer basin (240m min. thickness) comprises 10-15 sand packages (5-100m thick) formed by turbidite sands which are commonly amalgamated. Sedimentation in the Outer basin is considered to have been controlled by thrust-induced relative sea-level variations. The Inner basin underwent intense deformation at the sediment/water interface prior to the emplacement of a mud sheet over the basin whilst the sediments were partially lithified. Later tectonic deformation involved fold and thrust structures detaching in the underlying Globigerina marls. The stratigraphy of the NAFB can be considered as two shallowing upward megasequences separated by the base Burdigalian unconformity. This stratigraphy can be simulated by computer by simplifying the foreland basin/thrust wedge system into 4 parameters: 1) the effective elastic thickness of the foreland plate, 2) a transport coefficient to describe the erosion, transport and deposition of sediment, 3) the surface slope angle of the thrust wedge, 4) the thrust wedge advance rate. The Alpine thrust wedge underwent thickening during the underplating of the External Massifs at about 24-18Ma. This event is simulated numerically by slowing the thrust wedge advance rate, and increasing the slope angle and keeping all other parameters constant. This event causes rejuvenation of the forebulge, and erosion of the underlying stratigraphy, so simulating the base Burdigalian unconformity without recourse to eustasy or anelastic rheologies to the foreland plate.
APA, Harvard, Vancouver, ISO, and other styles
7

Rahman, Mohammad Wahidur Uddin Ashraf. "Sedimentation and tectonic evolution of Cenozoic sequences from Bengal and Assam foreland basins, eastern Himalayas." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SUMMER/Geology_and_Geography/Thesis/Rahman_Mohammad_54.pdf.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Jones, Neville Edward. "Controls on late stage fluvial systems in foreland basins : an example from the tertiary Digne-Valensole Basin of the external French Alps." Thesis, University of Liverpool, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367698.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Kollmann, Michael. "Strukturelle und sedimentologische Prozesse der Entwicklung eines Foreland-Basins das Zinda-Pir-Antiklinorium und die Sulaiman Range, Pakistan /." [S.l. : s.n.], 1999. http://deposit.ddb.de/cgi-bin/dokserv?idn=963754068.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Angrand, Paul. "Évolution 3D d'un rétro-bassin d'avant-pays : le Bassin aquitain, France." Thesis, Université de Lorraine, 2017. http://www.theses.fr/2017LORR0227/document.

Full text
Abstract:
Les bassins d'avant-pays se développent au front des orogènes par flexure de la lithosphère. L'héritage structural et thermique de celle-ci joue un rôle fondamental dans leur évolution et différentes sources peuvent contribuer à la subsidence du bassin. Cette thèse analyse les effets de l'héritage d'un épisode de rift sur un rétro-bassin d'avant-pays qui s'est développé alors que la lithosphère n'avait pas retrouvé son état d'équilibre. Le Bassin Aquitain est le rétro-bassin d'avant-pays pyrénéen qui s'est développé au Campanien-Miocène. L'orogenèse pyrénéenne fait suite à un épisode de rifting Aptien-Cénomanien durant lequel la croûte a été fortement amincie et le manteau sous-continental exhumé. Les effets de l'héritage crustal dus au rift sur l'évolution du bassin sont étudiés par une analyse des structures dans la croûte, du comportement flexural de la plaque européenne et de la distribution des sédiments synorogéniques. L'évolution de la subsidence dans le bassin est étudiée par analyse de subsidence 1D d'après des données de forages. Enfin, les mécanismes d'inversion de la marge européenne sont étudiés par restauration d'une coupe structurale à échelle crustale. Cette étude aide à définir le rôle de l'héritage d'un ancien système de rift sur la mise en place et l'évolution d'un bassin d'avant-pays ainsi que le rôle des différentes sources de subsidence et leurs variations spatio-temporelles. Cette étude démontre également les liens étroits entre l'histoire du rétro-bassin d'avant-pays et les mécanismes et phases d'inversion de la marge hyper-amincie
Foreland basins develop in front of orogens by flexure of the lithosphere. When they initiate over a crust that has been affected by a previous tectonic event, structural and thermal inheritance have a fundamental role in their evolution and different sources may contribute to basin subsidence. The present work analyzes the impact of inheritance from a rifting event on a foreland basin, which develops while thermal reequilibration has not been achieved at the time of loading. The Aquitaine Basin is the Pyrenean retro-foreland basin that developed from Campanian to Miocene. The Pyrenean orogenesis follows an Aptian-Cenomanian rifting during which the continental crust is thinned and sub-continental mantle exhumed. The orogenesis starts only 10 Myr after the end of rifting. The effects of crustal inheritance due to rifting on the evolution of the basin are studied by analyzing crustal structures, flexural behavior of the European plate, and foreland succession distribution. The subsidence evolution of the basin is studied by the 1D backstripping technique using borehole data. Finally, inversion mechanisms of the European margin are studied by cross-section construction and restoration at crustal scale. This study helps to define the role of rift inheritance on the initiation and the evolution of a retro-foreland basin, as well as the relative role of subsidence sources and their variations in space and time. The present work also shows the strong relationship between the retro-foreland basin's history and both mechanism and the history and mechanisms of inversion of a hyper-extended margin
APA, Harvard, Vancouver, ISO, and other styles
More sources

Books on the topic "Foreland basins"

1

Allen, P. A., and P. Homewood, eds. Foreland Basins. Oxford, UK: Blackwell Publishing Ltd., 1986. http://dx.doi.org/10.1002/9781444303810.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Lacombe, Olivier, François Roure, Jérôme Lavé, and Jaume Vergés, eds. Thrust Belts and Foreland Basins. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

France, Société géologique de, Lacombe Olivier, Sociedad Geológica de España, and Institut français du pétrole, eds. Thrust belts and foreland basins: From kinematics to hydrocarbon systems. Berlin: Springer, 2007.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
4

Pirouz, Mortaza. The geometry and sedimentary record of tectonics in the Neogene Zagros foreland basin. Genève: Département de Géologie et Paléontologie, Université de Genève, 2013.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
5

Pashin, Jack C. Reevaluation of the Bedford-Berea sequence in Ohio and adjacent states: Forced regression in a foreland basin. Boulder, Colo: Geological Society of America, 1995.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
6

Blackstone, D. L. Foreland compressional tectonics: Southern Bighorn Basin and adjacent areas, Wyoming. Laramie, Wyo: Geological Survey of Wyoming, 1986.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
7

Wadia Institute of Himalayan Geology., ed. Excursion guide: The Siwalik foreland basin, Dehra Dun-Nahan sector. Dehra Dun, India: Wadia Institute of Himalayan Geology, 1991.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
8

The Ordovician basin in the Puna of NW Argentina and N Chile: Geodynamic evolution from back-arc to foreland basin. Stuttgart: Schweizerbart, 1990.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
9

H. de la R. Winter. A cratonic-foreland model for Witwatersrand Basin-Development in a continental, back-arc, plate-tectonic setting. Johannesburg: University of the Witwatersrand, 1986.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
10

Workshop on Himalayan Foreland Basin with Reference to Pre-Siwalik Tertiaries (1998 Jammu, India). Himalayan foreland basin with special reference to pre-Siwalik tertiaries: Selected papers presented at the Workshop on Himalayan Foreland Basin with Reference to Pre-Siwalik Tertiaries : held at Jammu University, Jammu, India, 16-19, March, 1998. Edited by Kumar Kishor, Sahni Ashok, and Wadia Institute of Himalayan Geology. Dehradun, India: Wadia Institute of Himalayan Geology, 2000.

Find full text
APA, Harvard, Vancouver, ISO, and other styles
More sources

Book chapters on the topic "Foreland basins"

1

Barnolas, Antonio, Juan C. Larrasoaña, Victoriano Pujalte, Birger Schmitz, Francisco J. Sierro, María P. Mata, Bastiaan C. J. van den Berg, et al. "Alpine Foreland Basins." In The Geology of Iberia: A Geodynamic Approach, 7–59. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-11190-8_2.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Sinclair, Hugh. "Thrust Wedge/Foreland Basin Systems." In Tectonics of Sedimentary Basins, 522–37. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781444347166.ch26.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Ahmadhadi, Faram, Olivier Lacombe, and Jean-Marc Daniel. "Early Reactivation of Basement Faults in Central Zagros (SW Iran): Evidence from Pre-folding Fracture Populations in Asmari Formation and Lower Tertiary Paleogeography." In Thrust Belts and Foreland Basins, 205–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_11.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Rudkiewicz, Jean Luc, Shahram Sherkati, and Jean Letouzey. "Evolution of Maturity in Northern Fars and in the Izeh Zone (Iranian Zagros) and Link with Hydrocarbon Prospectivity." In Thrust Belts and Foreland Basins, 229–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_12.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Mouthereau, F., O. Lacombe, J. Tensi, N. Bellahsen, S. Kargar, and K. Amrouch. "Mechanical Constraints on the Development of the Zagros Folded Belt (Fars)." In Thrust Belts and Foreland Basins, 247–66. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_13.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Oveisi, Behnam, Jérôme Lavé, and Peter van der Beek. "Rates and Processes of Active Folding Evidenced by Pleistocene Terraces at the Central Zagros Front (Iran)." In Thrust Belts and Foreland Basins, 267–87. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_14.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Jahani, Salman, Jean-Paul Callot, Dominique Frizon de Lamotte, Jean Letouzey, and Pascale Leturmy. "The Salt Diapirs of the Eastern Fars Province (Zagros, Iran): A Brief Outline of their Past and Present." In Thrust Belts and Foreland Basins, 289–308. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_15.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Ellouz-Zimmermann, N., E. Deville, C. Müller, S. Lallemant, A. B. Subhani, and A. R. Tabreez. "Impact of Sedimentation on Convergent Margin Tectonics: Example of the Makran Accretionary Prism (Pakistan)." In Thrust Belts and Foreland Basins, 327–50. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_17.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Ellouz-Zimmermann, N., S. J. Lallemant, R. Castilla, N. Mouchot, P. Leturmy, A. Battani, C. Buret, et al. "Offshore Frontal Part of the Makran Accretionary Prism: The Chamak Survey (Pakistan)." In Thrust Belts and Foreland Basins, 351–66. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_18.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Tarapoanca, Mihai, Dorina Tambrea, Victor Avram, and Bogdan Popescu. "The Geometry of the South Leading Carpathian Thrust Line and the Moesia Boundary: The Role of Inherited Structures in Establishing a Transcurent Contact on the Concave Side of the Carpathians." In Thrust Belts and Foreland Basins, 369–84. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-69426-7_19.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Conference papers on the topic "Foreland basins"

1

Edmonds, Douglas, Elizabeth Hajek, Nic Downton, and Alexander B. Bryk. "AVULSION FLOW-PATH SELECTION ON RIVERS IN FORELAND BASINS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283573.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Zeng, Tongsheng, Qingcai Zeng, and Yonglin Ouyang. "Dual-scale tomographic inversion for static correction in Foreland Basins." In SEG Technical Program Expanded Abstracts 2017. Society of Exploration Geophysicists, 2017. http://dx.doi.org/10.1190/segam2017-17654536.1.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Swift, D. J. P., J. A. Thorne, and D. Nummedal. "Sequence Stratigraphy in Foreland Basins: Inferences From the Cretaceous Western Interior." In Offshore Technology Conference. Offshore Technology Conference, 1985. http://dx.doi.org/10.4043/4846-ms.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

Valenza, Jeffery M., and Douglas A. Edmonds. "HYBRID PROGRADATIONAL-ANNEXATIONAL AVULSION SIGNATURES IN MODERN AND ANCIENT FORELAND BASINS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359369.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Doglioni, C., and G. Mariotti. "On The Foreland Monoclines and Foredeeps in the Mediterranean Belts." 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/10.3997/2214-4609.201405979.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Poole, Forrest G., and Ricardo Amaya-Martínez. "COEVAL BASINS WITHIN EARLY MESOZOIC CORDILLERAN RETROARC FORELAND SYSTEM OF SONORA, MEXICO." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-313909.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Liu, Y., Y. Xie, Z. Zhang, X. Yang, Y. Tong, and Y. Xin. "Source Rocks and Oil & Gas Distribution of Foreland Basins in South America." In SPE Latin American and Caribbean Petroleum Engineering Conference. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/177236-ms.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Tyler, N. "Tectono-Stratigraphic Controls on Deltaic Reservoir Architecture and Recovery Response in Foreland Basins." In 5th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.116.065eng.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Waldron, John W. F., Shawna E. White, G. R. Dunning, and S. Andrew DuFrane. "PROVENANCE OF THE NEWFOUNDLAND APPALACHIAN FORELAND BASINS: IMPLICATIONS FOR TECTONICS OF THE LAURENTIAN MARGIN." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328589.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Sassi, W., and J. L. Rudkiewicz. "Computer Modelling of Petroleum Systems Along Regional Cross-Sections in Foreland and Fold-and-Thrustbelts." 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/10.3997/2214-4609.201405994.

Full text
APA, Harvard, Vancouver, ISO, and other styles

Reports on the topic "Foreland basins"

1

Joseph, Philippe, Yannick Callec, and Mary Ford. Dynamic Controls on Sedimentology and Reservoir - Architecture in the Alpine Foreland Basin. IFPEN, July 2012. http://dx.doi.org/10.2516/ifpen/2012001.

Full text
APA, Harvard, Vancouver, ISO, and other styles
2

Leckie, D. A., and G. C. Nadon. Evolution of fluvial landscapes in the Western Canada Foreland Basin: Late Jurassic to the modern. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/209372.

Full text
APA, Harvard, Vancouver, ISO, and other styles
3

Knight, R. D., J. M. Bednarski, E. Grunsky, and H. A. J. Russell. Portable XRF chemostratigraphy of a paleo-glacial foreland basin, the Nanaimo Lowlands, Vancouver Island, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299725.

Full text
APA, Harvard, Vancouver, ISO, and other styles
4

McMechan, M., B. Anderson, R. Creaser, and F. Ferri. Clasts from the past: latest Jurassic-earliest Cretaceous foreland basin conglomerates, northeast British Columbia and northwest Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221571.

Full text
APA, Harvard, Vancouver, ISO, and other styles
5

Irigoyen, M. V., M. E. Villeneuve, and F. Quigg. Calibration of a Neogene magnetostratigraphy by 40Ar-39Ar geochronology: the foreland basin strata of northern Mendoza Province, Argentina. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210360.

Full text
APA, Harvard, Vancouver, ISO, and other styles
6

Jerzykiewicz, T., and M. Labonte. Representation and Statistical Analysis of Directional Sedimentary Structures in the Uppermost Cretaceous - Paleocene of the Alberta Foreland Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132546.

Full text
APA, Harvard, Vancouver, ISO, and other styles
7

Lavoie, D. The Lacolle Breccia: the record of the destruction of the Late Ordovician carbonate foreland basin in southern Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212046.

Full text
APA, Harvard, Vancouver, ISO, and other styles
8

Grotzinger, J. P., C. Gamba, S. M. Pelechaty, and D. S. McCormick. Stratigraphy of a 1.9 Ga foreland basin shelf-to-slope transition: Bear Creek Group, Tinney Hills area of Kilohigok Basin, District of Mackenzie. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122646.

Full text
APA, Harvard, Vancouver, ISO, and other styles
9

Decker, P. L. Brookian sequence stratigraphic framework of the northern Colville foreland basin, central North Slope, Alaska (poster and presentation): DNR Spring Technical Review Meeting, Anchorage, April 21-22, 2010. Alaska Division of Geological & Geophysical Surveys, April 2010. http://dx.doi.org/10.14509/21861.

Full text
APA, Harvard, Vancouver, ISO, and other styles
10

Wartes, M. A., P. L. Decker, D. W. Houseknecht, R. J. Gillis, and D. L. LePain. Foreland basin response to Paleocene rejuvenation in the Brooks Range, northern Alaska (presentation): AAPG 3P Arctic, The Polar Petroleum Potential Conference & Exhibition, Halifax, Nova Scotia, Canada, August 30 - September 2, 2011. Alaska Division of Geological & Geophysical Surveys, August 2011. http://dx.doi.org/10.14509/29547.

Full text
APA, Harvard, Vancouver, ISO, and other styles
You might also be interested in the extended bibliographies on the topic 'Foreland basins' for particular source types:
Journal articles Dissertations / Theses Books
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography