Solonker ophiolite in Inner Mongolia, China: A late Permian continental margin-type ophiolite

To better constrain the Early Paleozoic tectonic evolution of the southwestern Arigin Sum-Xilinhot- Xing’an Block, we applied detrital zircon U-Pb dating on the

Triassic–Jurassic evolution of the eastern North China Craton: Insights from the Lushun-Dalian area, South Liaodong Peninsula, NE China... Triassic-Jurassic evolution of the

Petrogenesis and emplacement deformation of the 597 Late Triassic Dushan composite pluton in the Yanshan fold and thrust belt: Implications 598 for the tectonic settings of

The Sugetbrak basalts from northwestern Tarim Block of northwest China: Geochronology, geochemistry and implications for Rodinia breakup and ice age in the Late Neoproterozoic... The

Subsequently, central-eastern Inner Mongolia experienced uplift and erosion until the deposition of Late Jurassic volcanic rocks and the formation of Early Cretaceous

The Taiyuan Formation (near Yangquan City, Shanxi Province, China) is composed of a group of deposits of continental–oceanic interaction facies, consisting of sand- stone, dark

Abstract: The Oligocene deposits of the Ulantatal area in Inner Mongolia (China) contain among the richest mammalian faunas from Asia.. To date, only some parts of the rodent

Holotype (CNU-NXI-540c–p, part and counterpart), articulated specimen. Abbreviations: as, antennal spine; ba, basipodite; en, endopodite; ex, exopodite; mbc, median branchial