Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …

When and how continental crust formed and evolved to its current state is a fundamental
question regarding crust–mantle evolution and geodynamic regimes on the early Earth …

The peripheral or exterior subduction is known to drive the breakup of Rodinia; however, the
geodynamic driving mechanism remains controversial, which may result from the slab …

我国三个主要的古老陆块(华北, 华南和塔里木陆块) 都发育中-新元古代岩浆岩.
根据大量的同位素年代学资料, 华北陆块中-新元古代岩浆事件可以分为7 个阶段, 其中1.78 Ga …

U–Pb geochronology of magmatic and detrital zircons (Zenaga and Bou Azzer-El Graara
inliers, Anti-Atlas Belt, Morocco) and a reassessment of the published constraints suggest a …

As a micro-continent lying at the junction of the North China, Yangtze, and Tarim Cratons in
northwest China, the composition and tectonic-thermal history of the Qaidam Block not only …

Abstract The Pamir Plateau contains critical information on the tectonic evolution from the
Proto-to Paleo-Tethys. In this contribution, we report geochronology, geochemistry and Sr …

Abstract The late Neoproterozoic (~ 720–541 Ma) tectonic evolution of South China may
have included the development of a paleo-ocean basin (the South China Ocean Basin …

The positions of the Tarim Craton in two Precambrian supercontinents Columbia and
Rodinia still remain unknown or controversial, as the craton is largely covered by desert in …

Neoproterozoic tectonic evolution, magmatic activities, and sedimentary sequences are
fundamental in understanding the transition from the dispersing of Rodinian continents to …