Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

Subduction zones not only return oceanic lithosphere into the mantle, but are also sites
where chemical components are transferred from the downgoing plate back to the surface in …

西天山位于中亚造山带的西南缘, 经历了复杂的增生造山过程. 它也是标志塔里木地块北部被动
陆缘与西伯利亚地块南侧宽阔活动陆缘最后拼合的构造带. 根据近年来的研究进展 …

Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.
However, crustal signatures in the mantle source of basaltic rocks above subduction zones …

The Tian Shan of Central Asia is located in the southwestern part of the Central Asian
Orogenic Belt (CAOB, also known as the Central Asian Orogenic System or CAOS) …

Rutile is the most common naturally occurring titanium dioxide polymorph and is widely
distributed as an accessory mineral in metamorphic rocks ranging from greenschist to …

The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …

Geochemical and geochronological evidence was obtained from granitoids of the South
Tianshan orogen and adjacent regions, which consist of three individual tectonic domains …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

The composition of continental subduction-zone fluids varies dramatically from dilute
aqueous solutions at subsolidus conditions to hydrous silicate melts at supersolidus …