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 …

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 …

The amalgamation of South (SCB) and North China Blocks (NCB) along the Qinling‐Dabie
orogenic belt involved several stages of high pressure (HP)‐ultra high pressure (UHP) …

The Tongbai orogen is located in a key tectonic position linking the Qinling orogen to the
west and the Dabie-Sulu orogen to the east. This orogen comprises a Paleozoic …

Abstract The Qinling‐Tongbai‐Dabie‐Sulu orogenic belt comprises a Palaeozoic accretion‐
dominated system in the north and a Mesozoic collision‐dominated system in the south. A …

Abstract The Tongbai-Hong'an orogen is located in a key tectonic position linking the Qinling
orogen to the west and the Dabie-Sulu orogen to the east. Because the orogen preserves a …

Isobaric interference correction is essential for the precise in situ Hf isotopic measurement of
zircons; however, there is difficulty in doing a proper interference correction for zircons with …

The Lhasa terrane, the main tectonic component of the Himalayan–Tibetan orogen, has
received much attention as it records the entire history of the orogeny. The occurrence of …

Although petrologic data from the North Qinling orogen in central China have provided
essential information on the geodynamic history of the orogenic cycle, the timing of the …

Continent–continent collision between the North China Block (NCB) and South China Block
(SCB) took place along the Qinling–Tongbai–Hong'an–Dabie orogens during the Triassic. A …