Abstract The Central Asian Orogenic Belt (CAOB) is the largest accretionary orogen in the
world with considerable Phanerozoic juvenile crustal growth. The eastern segment of the …

The Asian continent consists of many continental blocks that assembled during the
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …

The time frame and detailed tectonic processes during the transition from the Paleo-Asian
Ocean to the Paleo-Pacific Ocean regimes have long been controversial. The Jiamusi Block …

Northeast (NE) China is located in the eastern Central Asian Orogenic Belt (CAOB) and
evolved from the amalgamation of several microcontinental blocks, which, from west to east …

Abstract The Daheishan Horst in Jilin Province, NE China, is the key geological unit that
links the Solonker-Xar Moron-Changchun and Changchun-Yanji sutures, which are …

Tectonic evolution models for the Cretaceous Russia Sikhote‐Alin and eastern NE China
continental margin and interior remain controversial. To understand the magmatic evolution …

NE China recorded the key tectonic evolution history of the Eurasian Plate from the
Paleozoic-Mesozoic collisional formation of the Central Asian Orogenic Belt to the Mesozoic …

Abstract The Lesser Xing'an–Zhangguangcai Range (LXZGCR) in NE China was
traditionally interpreted to be the eastern part of the Songliao–Xilinhot Accretionary Terrane …

This study presents new secondary-ion mass spectrometry (SIMS) rutile and laser ablation–
inductively coupled plasma–mass spectrometry (LA–ICP–MS) zircon U-Pb geochronological …

The tectonic evolution of the ancient Mudanjiang Ocean within the Central Asian Orogenic
Belt (CAOB), is strongly debated. The ocean played an important role in the amalgamation …