Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China
Abstract The Qinling Orogenic Belt (QOB) is located between the North China and South
China Blocks, and has been considered to have formed by the collision between these …
China Blocks, and has been considered to have formed by the collision between these …
Early Mesozoic magmatism and tectonic evolution of the Qinling Orogen: Implications for oblique continental collision
Abstract The Qinling Orogenic Belt in Central China is formed by an oblique continental
collision between the North China and South China Blocks. In this review, we summarize the …
collision between the North China and South China Blocks. In this review, we summarize the …
Origin and evolution of a porphyry-breccia system: Evidence from zircon U-Pb, molybdenite Re-Os geochronology, in situ sulfur isotope and trace elements of the …
Abstract The Qiyugou Au deposit, located in the Xiong'ershan ore cluster of central China,
consists of breccia pipe hosted Au ore bodies (> 60 t Au) and newly discovered porphyry ore …
consists of breccia pipe hosted Au ore bodies (> 60 t Au) and newly discovered porphyry ore …
Tectonic regime switchover of Triassic Western Qinling Orogen: Constraints from LA-ICP-MS zircon U–Pb geochronology and Lu–Hf isotope of Dangchuan intrusive …
Abstract The Qinling Orogenic Belt, linking the Kunlun and Qilian Mountains to the west and
continuing farther east to the Dabie Mountain, was assembled by the convergence and …
continuing farther east to the Dabie Mountain, was assembled by the convergence and …
Zircon Hf–isotopic mapping for understanding crustal architecture and metallogenesis in the Eastern Qinling Orogen
C Wang, J Deng, L Bagas, Q Wang - Gondwana Research, 2017 - Elsevier
Abstract The Eastern Qinling Orogen (EQO) is a major composite collisional zone located
between the North China and the Yangtze cratons. This contribution combines geological …
between the North China and the Yangtze cratons. This contribution combines geological …
Metamorphic evolution of the East Tethys tectonic domain and its tectonic implications
Q Zhang, X Gao, R Chen, Y Zheng - Science China Earth Sciences, 2023 - Springer
Abstract The China Central Orogenic System (CCOS), extending in an east-west direction in
the middle part of China, is composed of the Early Paleozoic Altyn-North Qilian-North …
the middle part of China, is composed of the Early Paleozoic Altyn-North Qilian-North …
Fluid and metal sources of the Wenquan porphyry molybdenum deposit, Western Qinling, NW China
The Wenquan porphyry moybdenium deposit, Western Qinling, NW China, with a resource
of 247 million tonnes at 0.048% Mo, formed during Triassic collision between South China …
of 247 million tonnes at 0.048% Mo, formed during Triassic collision between South China …
Nature and origin of Triassic igneous activity in the Western Qinling Orogen: The Wenquan composite pluton example
ABSTRACT The Western Qinling has been acknowledged to witness superimposed
orogeny including north subduction of Paleotethys ocean and collision between North China …
orogeny including north subduction of Paleotethys ocean and collision between North China …
Petrogenesis of granitoids in the Dewulu skarn copper deposit: Implications for the evolution of the Paleotethys ocean and mineralization in Western Qinling, China
KF Qiu, J Deng - Ore Geology Reviews, 2017 - Elsevier
The Tethyan tectonic domain hosts numerous world-class mineral deposits. Among these,
the Dewulu skarn copper deposit in Western Qinling, China belongs to the Paleotethys ore …
the Dewulu skarn copper deposit in Western Qinling, China belongs to the Paleotethys ore …
Coupled supercontinent–mantle plume events evidenced by oceanic plume record
The most dominant features in the present-day lower mantle are the two antipodal African
and Pacific large low-shear-velocity provinces (LLSVPs). How and when these two …
and Pacific large low-shear-velocity provinces (LLSVPs). How and when these two …