Tectonically Deformed Coal: Focus on Microstructures & Implications for Basin Evolution DOI

Manish Kumar Srivastava,

Kaushal Kishor, Alok K. Singh

et al.

Marine and Petroleum Geology, Journal Year: 2024, Volume and Issue: unknown, P. 107223 - 107223

Published: Nov. 1, 2024

Language: Английский

Correlation between cumulative horizontal extension and strike-slip displacement in releasing bends: Discrete element analysis DOI

Lunyan Wei,

Guiting Hou,

Siegfried Zhiqiang WU

et al.

Journal of Structural Geology, Journal Year: 2025, Volume and Issue: unknown, P. 105406 - 105406

Published: March 1, 2025

Language: Английский

Citations

0
Formation of the Shuixie Cu–Co ore district in response to structural reactivation during block rotation in the southeastern Tibetan Plateau DOI
Saisai Li, Hongrui Zhang,

Thomas G. Blenkinsop

et al.

Mineralium Deposita, Journal Year: 2025, Volume and Issue: unknown

Published: March 29, 2025

Language: Английский

Citations

0
Analyzing Recent Tectonic Activity Along the Karak Wadi Al Fayha Fault System Using Seismic, Earthquake, and Remote Sensing Data DOI Creative Commons
Mu’ayyad Al Hseinat, Malek AlZidaneen,

Ghassan Sweidan

et al.

Geosciences, Journal Year: 2025, Volume and Issue: 15(5), P. 177 - 177

Published: May 14, 2025

The Karak Wadi Al Fayha Fault (KWF) is a major NW-trending intraplate wrench fault system extending over 325 km from Western in Jordan to Saudi Arabia. Structurally linked the Precambrian Najd System, KWF has been previously mapped using field observations, gravity, magnetic, and reflection seismic methods. However, these approaches lacked vertical resolution necessary characterize its shallow structure, leaving influence on recent deposits surface topography poorly understood. This study employs sections integrated with Digital Elevation Model refine terrain analysis enhance mechanism solutions for determining regional stress pattern. Our results provide compelling evidence of KWF’s upward propagation into surface, as demonstrated by deformation uppermost Cretaceous Cenozoic successions, distinct geomorphic features Model, alignment earthquake epicenters along fault, active landslides associated movement. We suggest that reactivation influenced changing fields Late (Turonian) present. Northwestern Arabian plate undergone multiple tectonic transitions, including WNW–ESE compression Syrian Arc Fold-Belt (Turonian–Plio-Pleistocene) subsequent NNE–SSW extension Red Sea rifting (Neogene–present). suggests latest movements result continued activity Irbid Rift event (Eocene) Dead Transform since Miocene.

Language: Английский

Citations

0
Tectonically Deformed Coal: Focus on Microstructures & Implications for Basin Evolution DOI

Manish Kumar Srivastava,

Kaushal Kishor, Alok K. Singh

et al.

Marine and Petroleum Geology, Journal Year: 2024, Volume and Issue: unknown, P. 107223 - 107223

Published: Nov. 1, 2024

Language: Английский

Citations

1