[HTML][HTML] Sixty years of anisotropy of magnetic susceptibility in deformed sedimentary rocks
JM Parés - Frontiers in Earth Science, 2015 - frontiersin.org
The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …
Review of major shale-dominated detachment and thrust characteristics in the diagenetic zone: Part I, meso-and macro-scopic scale
There is considerable variability in the thickness, structure, and macroscopic deformation
style within shale-prone major thrust zones, which also impacts the structural style in the …
style within shale-prone major thrust zones, which also impacts the structural style in the …
Magnetostratigraphic data on Neogene growth folding in the foreland basin of the southern Tianshan Mountains
J Sun, Y Li, Z Zhang, B Fu - Geology, 2009 - pubs.geoscienceworld.org
Abstract The Tianshan Range is one of the longest and highest mountain belts in Central
Asia, stretching east-west for~ 2500 km. Uplift of this late Paleozoic orogenic belt resulted …
Asia, stretching east-west for~ 2500 km. Uplift of this late Paleozoic orogenic belt resulted …
Neogene uplift of the Tian Shan Mountains observed in the magnetic record of the Jingou River section (northwest China)
J Charreau, Y Chen, S Gilder, L Barrier… - …, 2009 - Wiley Online Library
The Tian Shan Mountains constitute central Asia's longest and highest mountain range.
Understanding their Cenozoic uplift history thus bears on mountain building processes in …
Understanding their Cenozoic uplift history thus bears on mountain building processes in …
Multi‐Phase Non‐Coaxial Orogenic Growth: Propagation of the Longmen Shan Thrust Belt on the Eastern Margin of the Tibetan Plateau
Reconstructing the deformation sequence and strain history of the Longmen Shan thrust belt
(LSTB) has significant implications for the growths of the SW Qinling orogenic belt and the …
(LSTB) has significant implications for the growths of the SW Qinling orogenic belt and the …
Paleoenvironmental significance of the magnetic fabrics in Chinese loess-paleosols since the last interglacial (< 130 ka)
R Zhu, Q Liu, MJ Jackson - Earth and Planetary Science Letters, 2004 - Elsevier
We compare new anisotropy of magnetic susceptibility (AMS) data with previously-
determined paleoclimatically sensitive parameters for a loess profile at Lingtai, central Loess …
determined paleoclimatically sensitive parameters for a loess profile at Lingtai, central Loess …
How deformed are weakly deformed mudrocks? Insights from magnetic anisotropy
JM Parés - Geological Society, London, Special Publications, 2004 - lyellcollection.org
For over thirty years the anisotropy of magnetic susceptibility (AMS) has been exploited in
rock fabric studies. Our knowledge of the mechanisms leading to magnetic fabric …
rock fabric studies. Our knowledge of the mechanisms leading to magnetic fabric …
The origin of tectonic lineation in extensional basins: combined neutron texture and magnetic analyses on “undeformed” clays
In extensional sedimentary basins fine-grained sediments that appear undeformed at the
outcrop scale can carry a magnetic fabric consistent with the regional deformation pattern …
outcrop scale can carry a magnetic fabric consistent with the regional deformation pattern …
Anisotropy of magnetic susceptibility in weakly deformed red beds from the Wyoming salient, Sevier thrust belt: Relations to layer-parallel shortening and orogenic …
Anisotropy of magnetic susceptibility (AMS) and structural studies of red beds in the
Wyoming salient were completed to evaluate relations of magnetic fabrics to layer-parallel …
Wyoming salient were completed to evaluate relations of magnetic fabrics to layer-parallel …
Kinematics of a former oceanic plate of the Neotethys revealed by deformation in the Ulukışla basin (Turkey)
Kinematic reconstruction of modern ocean basins shows that since Pangea breakup a vast
area in the Neotethyan realm was lost to subduction. Here we develop a first‐order …
area in the Neotethyan realm was lost to subduction. Here we develop a first‐order …