Origin of the Muguayuan veinlet-disseminated tungsten deposit, South China: Constraints from in-situ trace element analyses of scheelite

XY Li, JF Gao, RQ Zhang, JJ Lu, WH Chen, JW Wu - Ore Geology Reviews, 2018 - Elsevier
Abstract The Late Triassic Muguayuan W deposit is located in the middle of the Jiangnan
Orogen, South China. This deposit is characterized by veinlet-disseminated W …

Beyond Byerlee friction, weak faults and implications for slip behavior

C Collettini, T Tesei, MM Scuderi, BM Carpenter… - Earth and Planetary …, 2019 - Elsevier
Some faults are considered strong because their strength is consistent with the Coulomb
criterion under Byerlee's friction, 0.6< μ< 0.85. In marked contrast, numerous studies have …

Lateral middle-lower crustal flow in response to continental collision: New insights from the metamorphic complexes in the southeastern Tibetan Plateau

X Chen, J Liu, JP Burg, J Yan, B Zhou, H Shan… - Earth-Science …, 2023 - Elsevier
There have long been controversies over the extrusion mechanism of the Sundaland, block
in southeastern Tibetan Plateau in response to the tectonic convergence, between the …

The Ailao Shan–Red River shear zone revisited: Timing and tectonic implications

J Liu, X Chen, Y Tang, Z Song, W Wang - GSA Bulletin, 2020 - pubs.geoscienceworld.org
Continental strike-slip shear zones that may bear important information about the evolution
of convergent tectonics often occur to accommodate plate convergence. When and how …

Fluid overpressure from chemical reactions in serpentinite within the source region of deep episodic tremor

MS Tarling, SAF Smith, JM Scott - Nature Geoscience, 2019 - nature.com
Slow fault slip includes a range of transient phenomena that occur over timescales longer
than those of standard earthquakes. Slow slip events are often closely associated with …

Deformation at the frictional-viscous transition: Evidence for cycles of fluid-assisted embrittlement and ductile deformation in the granitoid crust

P Wehrens, A Berger, M Peters, T Spillmann… - Tectonophysics, 2016 - Elsevier
Mid-crustal deformation is classically characterized by the transition from ductile to brittle
deformation defining the frictional-to-viscous transition (FVT). Here we investigate an …

Fault geometry and fluid-rock reaction: Combined controls on mineralization in the Xinli gold deposit, Jiaodong Peninsula, China

L Yang, R Zhao, Q Wang, X Liu… - Journal of Structural …, 2018 - Elsevier
The structures and fluid-rock reaction in the Xinli gold deposit, Jiaodong Peninsula, were
investigated to further understand their combined controls on the development of …

[HTML][HTML] 造山型金矿构造控矿作用

杨林, 王庆飞, 赵世宇, 李华健, 赵鹤森, 董超一… - 岩石学报, 2023 - dzkx.org
造山型金矿具有重要经济价值, 其成矿理论研究对全球金矿勘查和开采具有重要意义.
为了更好的理解挤压和伸展背景下深成-中成-浅成造山型金矿成矿过程中控矿断裂形成过程 …

[HTML][HTML] 鲜水河断裂带乾宁段蠕滑变形及局部粘滑变形的岩石学记录

吴琼, 李海兵, 潘家伟, 米桂龙, 葛成隆, 赵中宝… - 岩石学报, 2023 - dzkx.org
鲜水河断裂带作为控制青藏高原物质大规模向东侧向挤出的北部边界, 是中国乃至世界上大陆
内部强震活动最频繁的断裂带之一, 但大地测量学研究表明它具有广泛的浅部蠕滑变形行为 …

[HTML][HTML] Fluid-mediated transition from dynamic rupturing to aseismic slip at the base of the seismogenic continental crust

A Ceccato, G Pennacchioni - Earth and Planetary Science Letters, 2025 - Elsevier
Chemo-mechanical fluid-rock interactions are critical in controlling the frictional-viscous
transition in the continental crust and the competition between seismic and aseismic …