[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses
P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …
geological framework and initial growth were fundamentally the result of multiple, previous …
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 …
Adakitic rocks at convergent plate boundaries: Compositions and petrogenesis
Q Wang, L Hao, X Zhang, J Zhou, J Wang, Q Li… - Science China Earth …, 2020 - Springer
Adakitic rocks are intermediate-acid magmatic rocks characterized by enrichment in light
rare-earth elements, depletion in heavy rare-earth elements, positive to negligible Eu and Sr …
rare-earth elements, depletion in heavy rare-earth elements, positive to negligible Eu and Sr …
Trace element discrimination of arc, slab failure, and A-type granitic rocks
JB Whalen, RS Hildebrand - Lithos, 2019 - Elsevier
Although widely used, classification schemes for granitic rocks have until now failed to
separate slab failure from arc magmatism in collisional orogens. Our previous work showed …
separate slab failure from arc magmatism in collisional orogens. Our previous work showed …
Petrogenesis of Middle–Late Triassic volcanic rocks from the Gangdese belt, southern Lhasa terrane: Implications for early subduction of Neo-Tethyan oceanic …
The Gangdese belt is dominantly composed of igneous rocks that formed during the
northward subduction of Neo-Tethyan oceanic lithosphere beneath the Lhasa terrane and …
northward subduction of Neo-Tethyan oceanic lithosphere beneath the Lhasa terrane and …
Post-collisional ultrapotassic mafic magmatism in South Tibet: Products of partial melting of pyroxenite in the mantle wedge induced by roll-back and delamination of …
Abstract Post-collisional (25–8 Ma) ultrapotassic mafic magmatic rocks occur to the north of
the India–Asia collision zone within the Lhasa terrane of the southern Tibetan Plateau …
the India–Asia collision zone within the Lhasa terrane of the southern Tibetan Plateau …
The Himalaya in 3D: Slab dynamics controlled mountain building and monsoon intensification
Tectonic models for the Oligocene–Miocene development of the Himalaya mountain range
are largely focused on crustal-scale processes, and developed along orogen-perpendicular …
are largely focused on crustal-scale processes, and developed along orogen-perpendicular …
Oceanic plateau subduction during closure of the Bangong-Nujiang Tethyan Ocean: Insights from central Tibetan volcanic rocks
LL Hao, Q Wang, C Zhang, Q Ou, JH Yang… - GSA …, 2019 - pubs.geoscienceworld.org
Identification of arc magmatic rock associations in a subduction zone has important
implications for specifically revealing the geodynamic evolution of the subduction system …
implications for specifically revealing the geodynamic evolution of the subduction system …
Late Pliocene onset of the Cona rift, eastern Himalaya, confirms eastward propagation of extension in Himalayan-Tibetan orogen
Several competing hypotheses have been proposed to explain east-west extension
observed across the Himalayan orogen, based primarily on observations from the western …
observed across the Himalayan orogen, based primarily on observations from the western …
[HTML][HTML] 青藏高原近南北向裂谷的时空分布特征及动力学机制
卞爽， 于志泉， 龚俊峰， 杨蓉， 程晓敢， 林秀斌… - 地质力学 …, 2021 - journal.geomech.ac.cn
青藏高原南部发育的一系列近南北向裂谷是印度-欧亚大陆持续挤压作用下的大型伸展构造,
也是揭示高原后碰撞构造演化过程的重要对象. 目前, 关于南北向裂谷的形成机制存在多种假说 …
也是揭示高原后碰撞构造演化过程的重要对象. 目前, 关于南北向裂谷的形成机制存在多种假说 …