This paper presents a review on the rock associations, geochemistry, and spatial distribution
of Mesozoic-Paleogene igneous rocks in Northeast Asia. The record of magmatism is used …

The formation of collisional orogens is a prominent feature in convergent plate margins. It is
generally a complex process involving multistage tectonism of compression and extension …

提要: 秦岭造山带以其独特的大地构造位置, 复杂的地质演化和丰富的矿产资源而成为地质科学
研究的焦点, 科学家已经基本清楚了其大地构造格局和地质演化轮廓, 共识其在印支期(三叠纪 …

The Phanerozoic tectonic regimes of the South China Block (SCB) hold a key to
understanding of its geodynamic evolution with respect to formation of numerous mineral …

Phanerozoic primary tin and tungsten deposits and lithium–cesium–tantalum (LCT) type
pegmatites define discontinuous belts that reach several thousand kilometers length …

Chemical geodynamics is an integrated discipline that studies the geochemical structure
and tectonic evolution of geospheres with the aim of linking tectonic processes to …

Regolith-hosted rare earth element (REE) deposits, also called ion-adsorption or weathered
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …

Crustal subduction and continental collision is the core of plate tectonics theory.
Understanding the formation and evolution of continental collision orogens is a key to …

The geochemical signatures of subducting crust have been identified in various types of
mafic igneous rocks at convergent plate boundaries, where island arc basalts (IAB) and …

Partial melting at continental lithosphere depths plays an important role in generating
geochemical variations in igneous rocks. In particular, dehydration melting of ultrahigh …