Anticipated frictional dissipation during seismic rupture is such (10–100 MW/m2) that melting
on fault planes should be widespread provided slip is well-localized. However, despite …

This paper discusses the results of field-based geological investigations of exhumed rocks
exposed in the Musgrave Ranges (Central Australia) and in Nusfjord (Lofoten, Norway) that …

Tectonic pseudotachylytes, ie quenched friction-induced silicate melts, record coseismic slip
along faults and are mainly reported from the brittle crust in association with cataclasites. In …

Thin (0.5–2 mm thick) pseudotachylyte veins occur within muscovite-bearing (∼ 10%
volume), amphibolite-facies quartzites of the Schneeberg Normal Fault Zone (Austroalpine …

在实验室使用红外热像仪和接触式测温仪同步观测记录了压性和张性雁列断层失稳错动前后的
热场变化过程. 从实验记录中发现, 在断层失稳引起温度场和热红外辐射亮温温度场上升之前 …

Sedimentary injectites hosted within basement rocks, where preserved on land, offer a
means to investigate the geometry, extent, dimensions and spacing of fractures that form an …

Pseudotachylytes are ubiquitous within New Zealand's Alpine Fault Zone, occurring as:(i)
thin fault veins parallel to existing hanging wall mylonitic foliation;(ii) thicker fault and …

The determination of the maximum temperature achieved by friction melt (Tmelt) in
pseudotachylytebearing faults is crucial to estimate earthquake source parameters (eg …

Abstract At Mt. Moncuni (Lanzo Massif, Western Alps) plagioclase peridotites and early mid-
ocean ridge basalt (MORB) gabbroic dykes are deformed by shear zones containing …

The mylonites of the Baccu Locci Shear Zone (BLSZ), Sardinia (Italy), were deformed during
thrusting along a bottom-to-top strain gradient in lower greenschist facies. The …