Search results
Results from the WOW.Com Content Network
Structural geology is the study of the three-dimensional distribution of rock units with respect to their deformational histories. The primary goal of structural geology is to use measurements of present-day rock geometries to uncover information about the history of deformation ( strain ) in the rocks, and ultimately, to understand the stress ...
Structural evolution of the Louisiana gulf coast; Stylolite; Subgrain rotation recrystallization; Suture (geology) Syncline; Syntaxis (geology) T. TaskForceMajella;
In structural geology, a suture is a joining along a major fault zone, of separate terranes, tectonic units that have different plate tectonic, metamorphic and paleogeographic histories. The suture is often represented on the surface by an orogen or mountain range. [1]
Ramsay's work in advancing structural geology was recognised by the awards of the Bigsby (1973) and Wollaston (1986) medals of the Geological Society of London, the Société Géologique de France Prestwich Medal in 1989, Sir Arthur Holmes Medal of the European Union of Geosciences (EGU) in 1984, C. T. Clough medal (1962) of the Edinburgh Geological Society, and the University of Liège medal ...
Among his awards and honors, he received the Best Publication Award in Structural Geology and Tectonics from the Geological Society of America in 1986 and 1996, the Alexander von Humboldt Foundation research prize in 2006, the Wilbur Lucius Cross Medal from the Yale Graduate School in 2007 and the Career Contribution Award in Structural Geology and Tectonics from the Geological Society of ...
In structural geology the term was first used to describe the thrust-bounded imbricates found within a thrust duplex. [2] In later literature it has become a general term for any block entirely bounded by faults, whether the overall deformation type is contractional , extensional or strike-slip in nature.
This is a compilation of the properties of different analog materials used to simulate deformational processes in structural geology. Such experiments are often called analog or analogue models. The organization of this page follows the review of rock analog materials in structural geology and tectonics of Reber et al. 2020. [1]
A pull-apart basin is a structural basin where two overlapping (en echelon) strike-slip faults or a fault bend create an area of crustal extension undergoing tension, which causes the basin to sink down. Frequently, the basins are rhombic or sigmoidal in shape. Dimensionally, basins are limited to the distance between the faults and the length ...