Metamorphic fluids, faults, and shear zones are carriers of carbon from the deep Earth to shallower reservoirs. Some of these fluids are reduced and transport energy sources, like …
PC England, AJ Smye - Geochemistry, Geophysics …, 2023 - Wiley Online Library
A thermal and mechanical framework is presented for analysis of pressure‐temperature (P‐ T) data and structural observations from high‐pressure‐low‐temperature (HPLT) terrains. P …
Typical rocks at shallow depths of seismogenic faults are fluid-rich gouges. During earthquakes, on-fault frictional heating may trigger thermal pressurization and dynamic fault …
Thermal pressurization (TP) is predicted to be an important dynamic frictional weakening mechanism during earthquakes. The prevailing models, though, assume that the physical …
D Gu, R Han, S Woo - Journal of Geophysical Research: Solid …, 2021 - Wiley Online Library
We conducted outcrop‐to‐nanoscale structural observations on a principal slip zone (PSZ) of the Yangsan fault, a major strike‐slip fault in southeast Korea, and some high‐velocity …
Exhumed faults in granitoids along the Lanterman Fault-Rennick Graben Fault system (northern Victoria Land, Antarctica) show superposed ductile to brittle deformation and …
Abstract The northern Adamello batholith (European Southern Alps) is crosscut by EW trending pseudotachylyte-bearing paleoseismic fault zones composed of multiple …
Tectonic pseudotachylytes are thought to be unique to certain water‐deficient seismogenic environments and their presence is considered to be rare in the geological record. Here, we …