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3 edition of Tectonic Control on the Hydrodynamics and Sedimentary Record of Extensional Basins found in the catalog.

Tectonic Control on the Hydrodynamics and Sedimentary Record of Extensional Basins

Ronald van Balen

Tectonic Control on the Hydrodynamics and Sedimentary Record of Extensional Basins

Inferences From Numerical Modelling and Analyses of the Pannonian Basin

by Ronald van Balen

  • 393 Want to read
  • 3 Currently reading

Published by Vrije Universitat .
Written in English


The Physical Object
FormatPaperback
Number of Pages202
ID Numbers
Open LibraryOL12852733M
ISBN 109090087044
OCLC/WorldCa69007180

You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read. Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them.,,,, Free ebooks since Steventon M, Jackson C, Hodgson D, Johnson H et al., , Strain analysis of a seismically-imaged mass-transport complex (MTC), offshore Uruguay, Basin Research, Vol: 31, Pages: , ISSN: X Strain style, magnitude, and distribution within mass-transport complexes (MTCs) is important for understanding the process evolution of submarine mass flows and for estimating their runout.

Blanc‐Valleron, M.M. () The salt basins of Alsace (Southern Rhine Graben). In: Sedimentary Deposition in Rift and Foreland Basins in France and Spain (Paleogene and Lower Neogene) (eds G. Brusson & B.C. Schreiber), pp 95 – Columbia University Press. AAPG ANNUAL CONFERENCE AND EXHIBITION Ideas and Innovation: Fuel for the Energy Capital. April , , Houston, Texas, USA Along-Strike Sediment Transport is an Underappreciated Control on the Pleistocene Sedimentary Record Offshore East Coast Trinidad. Jurassic and Cretaceous Sedimentary Fill of Intrashelf Basins of the Eastern.

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Tectonic Control on the Hydrodynamics and Sedimentary Record of Extensional Basins by Ronald van Balen Download PDF EPUB FB2

Request PDF | Extensional fault control on the sedimentation patterns in a continental rift basin: El Castellar Formation, Galve sub-basin, Spain | In the Galve sub-basin, the sedimentary record.

Normal faults commonly represent one of the principal controls on the origin and formation of sedimentary rock-hosted mineral deposits. Their presence within rift basins has a profound effect on fluid flow, with their impact ranging from acting as barriers, causing pressure compartmentalization of basinal pore fluids, to forming conduits for up-fault fluid flow.

The tidal hydrodynamics governing the strait results from a semi-diurnal phase inversion between two interlinked wider basins (i.e., the Tyrrhenian Sea to the north and the Ionian Sea to the south.

Alluvial-fluvial sedimentary successions unconformably overly volcanic rocks and the older turbidite sequences, and represent an important time marker in the evolution of the greenstone belts (Card, ). Alluvial-fluvial sedimentary rocks are distributed along major fault zones, where they occur as tectonic slices or as preserved synclinal keels.

Tectonic control on the hydrodynamics and sedimentary record of extensional basins; inferences from numerical modelling and analyses of the Pannonian Basin.

Diss. Diss. Vrije Univ. Amsterdam. pp., many figs. Orig. wrps. € The northern Sicily continental margin, in the southern Tyrrhenian Sea, extends from the north Sicily coastal belt to the Marsili bathyal plain (Fig.

1a).The margin is located in the transitional area between the Sicilian–Maghrebian chain to the south and the Tyrrhenian back-arc basin to the north (Kastens et al.,Scarascia et al., ).

Cited by: Obviously, regional tectonic studies and general plate tectonic configurations and processes were of great importance in the early stages, whereas the need to model basin subsidence and geometries paved the way for basin modelling of many by: Tectonic and climatic modes during extensional sedimentary basin evolution MIKE LEEDER School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK The competing effects of tectonics and climate on sedimentation in sedimentary basins are examined, with examples taken from the Quaternary of two active extensional provinces.

Abstract. Neo-tectonism affected the evolution of landscape across the earth since post-Miocene. The Khari river in Lower Damodar fan delta in West Bengal similarly portrayed the imprints of neo-tectonism in the forms of rapidly changing meander geometry, deformation in long profiles, unpaired terraces, soft sediment structures (fluid escape structure and convolute), : Suman Deb Barman, Aznarul Islam, Balai Chandra Das, Sunipa Mandal, Subodh Chandra Pal.

Cambridge Core - Sedimentology and Stratigraphy - Earth Surface Processes, Landforms and Sediment Deposits - by John BridgeCited by:   Outcrop analysis and facies model of an Upper Permian tidally influenced fluvio-deltaic system: Northern Sydney Basin, SE Australia - Volume Issue 10 - Jake Breckenridge, Angelos G.

Maravelis, Octavian Catuneanu, Kevin Ruming, Erin Holmes, William J. Collins. Age control on sedimentary sequences: A prospective sequence in the northern Arafura Basin, NT: Preliminary interpretations of BMR and industry seismic from sedimentary basins in eastern Australia: Palaeogeographic, palaeoenvironmental, and age controls on the composition of petroleum source rocks and their derived oils: Data Repository items are published exactly as the author provided them to the journal; they are not formatted or edited.

For further information about any Data Repository item, please contact the author. The Data Repository is an archive and has limited navigation and log-in functionality. Click on the GSA logo to return to the main site. Spring mounds on Earth and on Mars could represent optimal niches of life development.

If life ever occurred on Mars, ancient spring deposits would be excellent localities to search for morphological or chemical remnants of an ancient biosphere. In this work, we investigate models of formation and activity of well-exposed spring mounds in the Mechertate-Chrita-Sidi El Hani (MCSH) system Cited by: 5.

Welcome to the Thermocene: the potential impact of global warming on the sedimentary record: Oral: Nopola, Jay R.; Samuel J. Voegeli: Development of Thermal Breakout Technology for Determining the Maximum Horizontal In Situ Stress: Oral: Noyahr, Christopher; John A.

Weissenberger, Nicholas B. Harris, Jonathan C. Banks. Sedimentary Record of the Early-Middle Jurassic Inception of the Gulf of Mexico in Tlaxiaco Basin, Alberto Osmar Vite del Angel and J.

Rueda-Gaxiola, # (). Guadalupian Paleobiogeography across the Neotethys Ocean, Lucia Angiolini, Giovanni. Magmatic intrusions affect the basin temperature in their vicinity.

Faulting and physical properties of the basin may influence the magnitudes of their thermal effects and the potential source rock maturation.

We present results from a sensitivity study of the most important factors affecting the thermal history in structurally complex sedimentary basins with magmatic sill by: 1.

Most of those projects, however, focused on the central part of the basin, characterized by the thickest and most complete sedimentary record. The record there is dominated by fine‐grained strata of the Lockatong and Passaic Formations that have long been recognized as largely lacustrine in origin [ Van Houten, ; Olsen et al., Cited by: 1.

Deposition in these basins resulted in the production of thick sediment wedges. Using the modelling results from the West African Margin, together with palaeontological and stratigraphic correlations, the tectonic history of the rift basins comprising the eastern Brazilian Margin (i.e.

Jequitinhonha to Sergipe-Alagoas) can be inferred. The first order control on growth patterns and carbonate platform development by the regional plate-tectonic setting, underlying basin architecture and fluctuations in sea level will be illustrated.

The organisms that contribute to sequence development will be revealed to. 3D simulations of stratigraphic and sedimentary processes provided maps of net sand thickness and seal distribution all over the basin.

A subtle tectonic event was identified defining a new potential play in the Madre de Dios basin originating from a mild regional structuration inducing structural traps.C Workshop White Papers. SCIENTIFIC OCEAN DRILLING: PAST, PRESENT AND FUTURE.

Ted Moore University of Michigan. U.S. oceanographic institutions banded together in to take the first steps toward exploring the sedimentary record and the crustal rocks of the deep ocean basins.Suggested Citation: "3. Facing the Earthquake Threat." National Research Council.

Living on an Active Earth: Perspectives on Earthquake Science. Washington, DC: The National Academies Press.

doi: / FIGURE Many apartment buildings on the fringe of the river delta at Golcuk, Turkey, slid into the sea during the Izmit.