Central China orogenic belt and amalgamation of East Asian continents
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 …
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …
Cross Orogenic Belts in Central China: Implications for the tectonic and paleogeographic evolution of the East Asian continental collage
Abstract The East Asian continent records a complex geologic and tectonic history that
involved the amalgamation of several small-to medium-sized blocks from Laurasia or …
involved the amalgamation of several small-to medium-sized blocks from Laurasia or …
[HTML][HTML] Co-evolution of the Cenozoic tectonics, geomorphology, environment and ecosystem in the Qinling Mountains and adjacent areas, Central China
Abstract The Qinling Mountains stretching from east to west in Central China are an
important geological and geographical boundary in the China Continent and even the East …
important geological and geographical boundary in the China Continent and even the East …
Revisiting Phanerozoic evolution of the Qinling Orogen (East Tethys) with perspectives of detrital zircon
This paper presents 5383 detrital zircon U–Pb and 2079 Lu–Hf isotopic data, shedding new
light on the Phanerozoic tectonic evolution of the Qinling Orogen. The Silurian rocks are …
light on the Phanerozoic tectonic evolution of the Qinling Orogen. The Silurian rocks are …
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 …
Middle Triassic transcontinental connection between the North China Craton and the Paleo-Tethys Ocean
Middle Triassic paleogeography is essential for the paleoclimate change and ecosystem
recovery after the end-Permian mass extinction, but is highly debated in the Paleo-Tethys …
recovery after the end-Permian mass extinction, but is highly debated in the Paleo-Tethys …
Prototethyan orogenesis in southwest Yunnan and Southeast Asia
Abstract The Prototethyan Ocean has been suggested as an Early Paleozoic Ocean
developed at the Gondwana northern margin. However, its spatial pattern, subduction style …
developed at the Gondwana northern margin. However, its spatial pattern, subduction style …
Ordovician tectonic transition from passive margin into peripheral foreland in the southern Ordos: A diagnostic insight into the closure of Erlangping Ocean between …
Achieving a reliable closure time of a back‐arc ocean is an essential aspect in studies on
detailed tectonic processes of an active continental margin and arc–continent collision. This …
detailed tectonic processes of an active continental margin and arc–continent collision. This …
Detrital zircons from high-pressure trench sediments (Qilian Orogen): constraints on continental-arc accretion, subduction initiation and polarity of the Proto-Tethys …
Abstract The Qilian Orogen in the northern Tibetan plateau records the tectonic history of the
Proto-Tethys Ocean from its initial spreading, subduction to final closure. However, the …
Proto-Tethys Ocean from its initial spreading, subduction to final closure. However, the …
Linking environmental changes and organic matter enrichment in the middle part of the Yanchang Formation (Ordos Basin, China) to the rollback of an oceanic slab in …
J Zhang, Z Qiu, S Li, S Gao, R Guo, X Ma, J Qiu, S Li… - Sedimentary …, 2023 - Elsevier
Abstract The Yanchang Formation, which records the whole evolutionary history of the
Middle–Late Triassic lacustrine basin in the western part of the North China Block, provides …
Middle–Late Triassic lacustrine basin in the western part of the North China Block, provides …