What caused the denudation of the Menderes Massif: Review of crustal evolution, lithosphere structure, and dynamic topography in southwest Turkey
The deformation of Earth's lithosphere in orogenic belts is largely forced externally by the
sinking slab, but can also be driven by internal delamination processes caused by …
sinking slab, but can also be driven by internal delamination processes caused by …
Mesoarchean assembly and stabilization of the eastern Kaapvaal craton: A structural‐thermochronological perspective
B Schoene, MJ de Wit, SA Bowring - Tectonics, 2008 - Wiley Online Library
Understanding the construction and stabilization of Archean continental lithosphere has
important implications for models of tectonic and thermal regimes in the early Earth, as well …
important implications for models of tectonic and thermal regimes in the early Earth, as well …
[HTML][HTML] Early Cretaceous overprinting of the Mesozoic Daqing Shan fold-and-thrust belt by the Hohhot metamorphic core complex, Inner Mongolia, China
GA Davis, BJ Darby - Geoscience Frontiers, 2010 - Elsevier
The Early Cretaceous Hohhot metamorphic core complex (mcc) of the Daqing Shan (Mtns.)
of central Inner Mongolia is among the best exposed and most spectacular of the spatially …
of central Inner Mongolia is among the best exposed and most spectacular of the spatially …
Subduction polarity reversal at the junction between the Western Alps and the Northern Apennines, Italy
The controversial relationship between the orogenic segments of the Western Alps and the
Northern Apennines is here explored integrating recently published 3D tomographic models …
Northern Apennines is here explored integrating recently published 3D tomographic models …
General shear deformation in the Pinaleno Mountains metamorphic core complex, Arizona
CM Bailey, EL Eyster - Journal of Structural Geology, 2003 - Elsevier
Granitic mylonites from the Pinaleño Mountains metamorphic core complex in southeastern
Arizona record general shear deformation. The mean kinematic vorticity number (Wm) was …
Arizona record general shear deformation. The mean kinematic vorticity number (Wm) was …
Sheath folds as discriminators of bulk strain type
Nested elliptical closures defining “eye-folds” represent classic (y–z) cross sections through
highly curvilinear sheath folds generated during intense ductile deformation in metamorphic …
highly curvilinear sheath folds generated during intense ductile deformation in metamorphic …
Gliding and overthrust nappe tectonics of the Barberton Greenstone Belt revisited: A review of deformation styles and processes
MJ Van Kranendonk - South African Journal of Geology 2021, 2021 - journals.co.za
Abstract Interpretations of the structural/tectonic evolution of the Barberton Greenstone Belt
(BGB) and its surrounding granitoid rocks remain controversial, with proponents for both …
(BGB) and its surrounding granitoid rocks remain controversial, with proponents for both …
Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: polystage convergence and extension in the lower orogenic crust
The Grenville orogenic cycle, between∼ 1190 and 980 Ma, involved accretion of magmatic
arcs and/or continental terranes to the Laurentian craton. A transect across the western …
arcs and/or continental terranes to the Laurentian craton. A transect across the western …
Neogene structural evolution of the Sierra San Felipe, Baja California: Evidence for proto-gulf transtension in the Gulf Extensional Province?
The Sierra San Felipe, located in the Gulf Extensional Province of northeastern Baja
California, experienced a complex deformation history of integrated normal and strike-slip …
California, experienced a complex deformation history of integrated normal and strike-slip …
The geometry and topology of natural sheath folds: a new tool for structural analysis
Curvilinear sheath folds are classically depicted as displaying symmetrical geometries about
two orthogonal mirror planes centred along the (X–Y) axial surface and the (X–Z) medial …
two orthogonal mirror planes centred along the (X–Y) axial surface and the (X–Z) medial …