Results 181 to 190 of about 4,458,046 (219)
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, 2010
The southern Songliao Basin manifests itself as a wide-rift system that developed in northeast China from the Late Jurassic to Early Cretaceous.
Hong Wei, Junlai Liu, Q. Meng
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The southern Songliao Basin manifests itself as a wide-rift system that developed in northeast China from the Late Jurassic to Early Cretaceous.
Hong Wei, Junlai Liu, Q. Meng
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Application of Magnetics to Basin Structures
Proceedings, 1995Magnetic surveys have long been part of basin exploration but the use has either been for reconnaissance purposes, basement depth estimates, general mapping applications or some detailed review of isolated features. The data have been generally underutilised.
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Structure of the Western Mediterranean Basin
1974The purpose of this paper is to describe margins of some Western Mediterranean basin zones that have played a particular tectonic role during the Oligo-Miocene phases of creation of the basin or that have undergone recent tectonic activity. In the following description, five zones will be considered: Ligurian Sea, Gulf of Valencia, Alboran Sea ...
Jean-Louis Olivet, Jean-Marie Auzende
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, 2010
Luanping basin is one of many small rift basins that developed in northeast China during mid‐Cretaceous time. It is filled by alluvial, fan‐deltaic and lacustrine strata of the Lower Cretaceous (post 130 Ma) Xiguayuan Formation.
T. Cope +6 more
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Luanping basin is one of many small rift basins that developed in northeast China during mid‐Cretaceous time. It is filled by alluvial, fan‐deltaic and lacustrine strata of the Lower Cretaceous (post 130 Ma) Xiguayuan Formation.
T. Cope +6 more
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The structure of the Dead Sea basin
Tectonophysics, 1996Abstract The Dead Sea basin is located along the left-lateral transform boundary between the Arabian and Sinai plates. Its structure and history are known from surface geology, drilling, seismic reflection and other geophysical data. The basin comprises a large pull-apart, almost 150 km long and mostly 8–10 km wide, which is flanked by a few ...
Zvi Ben-Avraham, Zvi Garfunkel
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Venezuela Basin crustal structure
Journal of Geophysical Research: Solid Earth, 1981Velocity‐depth profiles derived from six two‐ship expanding spread experiments, in combination with other geophysical data, define the characteristics of two distinct types of Venezuela Basin crust and the boundary between them. Each two‐ship common midpoint reflection/refraction profile is automatically transformed into the τ‐p plane, ‘picked’ and ...
John B. Diebold +3 more
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The structure of basins of attraction and their trapping regions
Ergodic Theory and Dynamical Systems, 1997In dynamical systems examples are common in which two or more attractors coexist, and in such cases, the basin boundary is nonempty. When there are three basins of attraction, is it possible that every boundary point of one basin is on the boundary of the two remaining basins? Is it possible that all three boundaries of these basins coincide? When this
Helena E. Nusse, James A. Yorke
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Structural and basin evolution in Miocene time, southwestern Gulf of Suez, Egypt
, 2009Seismic-facies analysis and the subsurface tectonic evolution of the Western Sub-Basin (WSB)oftheGulfofSuez,Egypt,werestudiedbyseismicreflectiondataof45seismiclines.Eight of these lines were selected to illustrate the structural framework and ...
A. El-Naby +4 more
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Origin and structure of the Basin ranges
Geological Society of America Bulletin, 1901Introduction Investigation of the structure of the desert ranges which lie between the Wasatch and the Sierra and extend southward into California is no easy task. In the past different views have been held, some seeing in them a series of parallel folds in which the anticlines protruding above the surface formed the ranges, while others considered ...
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, 2009
The structural evolution of the Miocene to Recent Gediz Graben is intimately related to the evolution of its southern margin. This margin is shaped by a time‐transgressive, composite structure that possesses flat‐ramp geometry with three separate dip ...
N. B. Çiftçi, E. Bozkurt
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The structural evolution of the Miocene to Recent Gediz Graben is intimately related to the evolution of its southern margin. This margin is shaped by a time‐transgressive, composite structure that possesses flat‐ramp geometry with three separate dip ...
N. B. Çiftçi, E. Bozkurt
semanticscholar +1 more source