Early Stages Arc Volcanism in the Eastern Himalayan Synstaxis, Yarlung Zongbo Suture Zone, Tibet, China: New Zircon Age, Hf Isotopic, Geochemical Constrains and Implication for the Tectonic Evolution History of Neo-Tethys
Early Stages Arc Volcanism in the Eastern Himalayan Synstaxis, Yarlung Zongbo Suture Zone, Tibet, China: New Zircon Age, Hf Isotopic, Geochemical Constrains and Implication for the Tectonic Evolution History of Neo-Tethys
摘要
The Yarlung Zongbo Suture Zone （YZSZ） is thought to be the most important geological boundary, the collision between the India plate and the Eurasia happened since Cretaceous-Tertiary （Aitchison et al., 2011）. The YZSZ, bordered to the north by the Lhasa Block and to the south by the Tethyan sedimentary sequence and the Greater Himalaya, is exposed and dominated by the ophiolite complexes, the ophiolitic mdlange,
The Yarlung Zongbo Suture Zone （YZSZ） is thought to be the most important geological boundary, the collision between the India plate and the Eurasia happened since Cretaceous-Tertiary （Aitchison et al., 2011）. The YZSZ, bordered to the north by the Lhasa Block and to the south by the Tethyan sedimentary sequence and the Greater Himalaya, is exposed and dominated by the ophiolite complexes, the ophiolitic mdlange,
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