Metamorphic evolution and age constraints of the garnet-bearing mica schist from the Xindaduo area of the Sumdo (U)HP metamorphic belt, Tibet

As one of the major components of the Himalayan–Tibetan Orogeny, the Lhasa terrane plays a key role in understanding the origin and evolution of this giant orogenic belt and the opening and closure of the Tethys oceans. The eclogite-bearing Sumdo Complex in the central Lhasa terrane was recognized a...

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Veröffentlicht in:	Geological magazine 2019-07, Vol.156 (7), p.1175-1189
Hauptverfasser:	ZHANG, CONG, BADER, THOMAS, ZHANG, LINGMIN, SHEN, TINGTING, LI, PENG, LI, XUPING
Format:	Artikel
Sprache:	eng
Schlagworte:	Age Aggregation Amphibolites Asia Bangong-Nujiang suture zone Bearing Biological evolution chemical composition China Constraints dates Dating techniques Decompression Eclogite Evolution exhumation Far East Garnet garnet group Geology Heating Himalayan Orogeny Himalayas ICP mass spectra igneous and metamorphic rocks Indus-Yarlung Zangbo suture zone isotherms Isotopes Lhasa Block Magma mass spectra metamorphic belts metamorphic rocks Metamorphism Metamorphism (geology) Mica mica group nesosilicates Oceans Original Article orogenic belts Orogeny orthosilicates P-T conditions Paleoceanography Paleotethys Petrology Phase equilibria phengite Radiometric dating Researchers Schist Schists sheet silicates silicates spectra Structural geology Sumdo Belt Sumdo Complex suture zones Tectonics terranes U/Pb Xizang China
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