Results 211 to 220 of about 22,109 (259)
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Salt Tectonics

1995
Abstract The conceptual breakthroughs in understanding salt tectonics can be recognized by reviewing the history of salt tectonics, which divides naturally into three parts: the pioneering era, the fluid era, and the brittle era. The pioneering era (1856-1933) featured the search for a general hypothesis of salt diapirism,
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Retrospective Salt Tectonics

1995
The conceptual breakthroughs in understanding salt tectonics can be recognized by reviewing the history of salt tectonics, which divides naturally into three parts: the pioneering era, the fluid era, and the brittle era. The pioneering era (1856-1933) featured the search for a general hypothesis of salt diapirism, initially dominated by bizarre ...
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3D Numerical Modelling of Salt Tectonics

Proceedings, 2017
Summary Many factors have been suggested to affect the development of salt structures, including sedimentation, brittle sediment deformation, multiple tectonic events and basement topography. To unravel the relative importance of these processes, we performed high resolution 2D and 3D thermo-mechanical simulations that take these factors into account ...
Baumann, T.S.   +2 more
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Salt Tectonics

Scientific American, 1987
Christopher J. Talbot   +1 more
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Model Studies of Salt-Dome Tectonics

AAPG Bulletin, 1955
In a great many models constructed of various materials and analyzed in accordance with the theory of scale models, asphalt was the most nearly satisfactory material found to represent the salt, and weak muds of greater density than the asphalt were found to be best suited to represent the sedimentary overburden above the salt.
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Coupling Crustal‐Scale Rift Architecture With Passive Margin Salt Tectonics: A Geodynamic Modeling Approach

Journal of Geophysical Research: Solid Earth, 2022
Leonardo Muniz Pichel   +2 more
exaly  

Late‐Syn‐ to Post‐Rift Salt Tectonics on Wide Rifted Margins—Insights From Geodynamic Modeling

Tectonics, 2022
Leonardo Muniz Pichel   +2 more
exaly  

Salt-Tectonic Features of Northern Iraq

1968
Structural disharmonies between rock masses lying above and below the salt-bearing Lower Fars formation are characteristic of the Alpine foothill folds of the Zagros mountain belt in parts of northern Iraq and southwestern Iran. Most impressive and what appear to be chaotic structural discrepancies have been described from the Iran ...
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Salt tectonics

Tectonophysics, 1989
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Salt tectonics

Journal of Structural Geology, 1996
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