Faulting processes unveiled by magnetic properties of fault rocks
As iron‐bearing minerals—ferrimagnetic minerals in particular—are sensitive to stress,
temperature, and presence of fluids in fault zones, their magnetic properties provide …
temperature, and presence of fluids in fault zones, their magnetic properties provide …
[HTML][HTML] Magnetic fabric separation and analysis of rock tectonic deformation
Both detailed rock magnetism and structural analysis suggest that the routine anisotropy of
magnetic susceptibility (AMS) measurements can not suffice for the interpretations of …
magnetic susceptibility (AMS) measurements can not suffice for the interpretations of …
Back-thrusting response of continental collision: Early Cretaceous NW-directed thrusting in the Changle-Nan'ao belt (Southeast China)
The SE coastal area of the South China Block (SCB) is generally interpreted as a
Cretaceous active continental margin due to subduction of the Paleo-Pacific plate beneath …
Cretaceous active continental margin due to subduction of the Paleo-Pacific plate beneath …
An early extensional event of the South China Block during the Late Mesozoic recorded by the emplacement of the Late Jurassic syntectonic Hengshan Composite …
Continental scaled extension is the major Late Mesozoic (Jurassic and Cretaceous) tectonic
event in East Asia, characterized by faulting, magmatic intrusions and half-grabens in an …
event in East Asia, characterized by faulting, magmatic intrusions and half-grabens in an …
The deformed alkaline Balda granite (Northern Cameroon): A witness of back-arc basin in the northern part of Central African Orogenic Belt
A Bello, D Dawaï, PYJ Antonio, O Laurent… - Precambrian …, 2024 - Elsevier
Located on the border between the NW Cameroon and Mayo-Kebbi domains in northern
Cameroon, the Balda pluton is a deformed alkaline granite. Due to its unique location and …
Cameroon, the Balda pluton is a deformed alkaline granite. Due to its unique location and …
Unravelling textural heterogeneity in obsidian: Shear-induced outgassing in the Rocche Rosse flow
Obsidian flow emplacement is a complex and understudied aspect of silicic volcanism. Of
particular importance is the question of how highly viscous magma can lose sufficient gas in …
particular importance is the question of how highly viscous magma can lose sufficient gas in …
Use of magnetic fabrics and X-ray diffraction to reveal low strains in experimentally deformed Maggia gneiss
In this pilot study, we analyzed the response of magnetic fabrics and X-ray diffraction to low
strains (≤ 0.0103) applied during quasi-static and dynamic deformation. Four cylindrical …
strains (≤ 0.0103) applied during quasi-static and dynamic deformation. Four cylindrical …
Orogen‐parallel deformation of the Himalayan midcrust: Insights from structural and magnetic fabric analyses of the Greater Himalayan Sequence, Annapurna …
The metamorphic core of the Himalaya (Greater Himalayan Sequence, GHS), in the
Annapurna‐Dhaulagiri region, central Nepal, recorded orogen‐parallel stretching during …
Annapurna‐Dhaulagiri region, central Nepal, recorded orogen‐parallel stretching during …
The Late Jurassic extensional event in the central part of the South China Block–evidence from the Laoshan'ao shear zone and Xiangdong Tungsten deposit (Hunan …
ABSTRACT The Late Mesozoic tectonics strongly reworked the tectonic framework of East
Asia. In the South China Block (SCB), the major Late Mesozoic phenomena are featured by …
Asia. In the South China Block (SCB), the major Late Mesozoic phenomena are featured by …
Late Triassic contractional tectonics in the overriding plate of the Sulu orogenic belt, Eastern China
L Meng, W Lin - Tectonophysics, 2021 - Elsevier
It is well known that the Dabie-Sulu orogenic belt resulted from the northward continental
subduction of the South China Block (SCB) beneath the North China Block (NCB) during the …
subduction of the South China Block (SCB) beneath the North China Block (NCB) during the …