GEOLOGICAL CHARACTER AND SIGNIFICANCE OF ADAKITE AND TTG IN XIAONANGOU-MINGXINGGOU DISTRICT IN CENTRAL OF INNER MONGOLIA

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dc.contributor.author Zhang Y.Q.
dc.contributor.author Zhang Y.K.
dc.contributor.author Zheng B.J.
dc.contributor.author Han J.G.
dc.contributor.author Xu G.Q.
dc.contributor.author Mu J.J.
dc.contributor.author Zhang L.Q.
dc.date.accessioned 2024-09-04T09:55:43Z
dc.date.available 2024-09-04T09:55:43Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=31920825
dc.identifier.citation Acta Petrologica Sinica, 2006, 22, 11, 2762-2768
dc.identifier.issn 1000-0569
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44946
dc.description.abstract A suit of schistositied quartz diorite and schistositied tonalite in Neoarchean, which is exposed in Xiaonangou-Mingxinggou district in central of Inner Mongolia. Petrochemical contents show that it possesses high contents of SiO2, Al2O3, Na2O,Ba,Sr,Mg#,LREE and low contents of Yb,Y,HREE, and it possess the character of Adakite and TTG. It is associated intently with greenstone of Seertengshan Group Neoarchean in space distribution. The two isochronal age of zircon in quartz diorite are 2575 ± 1Ma (U-Pb) and 2541 ± 30Ma (U-Pb), it is formed by partial melting of ocean slab which formed on the belt of plate subduction in Neoarchean. It possesses important significance in studying early Earth evolution and origin of plate tectonics.
dc.subject ADAKITE
dc.subject INNER MONGOLIA
dc.subject QUARTZ DIORITE
dc.subject TONALITE
dc.subject TTG
dc.subject XIAONANGOU-MINGXINGGOU
dc.title GEOLOGICAL CHARACTER AND SIGNIFICANCE OF ADAKITE AND TTG IN XIAONANGOU-MINGXINGGOU DISTRICT IN CENTRAL OF INNER MONGOLIA
dc.type Статья
dc.subject.age Докембрий::Архей::Неоархейская
dc.subject.age Докембрий::Архей::Эоархейская
dc.subject.age Precambrian::Archean::Neoarchean
dc.subject.age Precambrian::Archean::Eoarchean


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