Age and origin of the Takeshiken postorogenic alkali-rich intrusive rocks in southern Altai, near the Mongolian border in China and its implications for continental growth;阿 尔 泰 中 蒙 边 界 塔 克 什 肯 口 岸 后 造 山 富 碱 侵 入 岩 体 的形 成 时 代 、 成 因 及 其 地 壳 生 长 意 义

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 22, Issue 5, 2006, Pages 1267-1278

  Tong, Ying ^a   Wang, Tao ^a   Vp, Kovach ^b   Hong, DaWei ^a   Han, BaoFu ^c  

^a INSTITUTE OF GEOLOGY   (China)

^b INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

^c PEKING UNIVERSITY   (China)

Author keywords

Alkali rich intrusive rock; Central Asian Orogenic Belt; Crustal growth; Nd isotope; Postorogenic; Zircon U Pb age

Indexed keywords

EID: 85178289670     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/a699084a3e9a436ea3126dd6625b179a     Document Type: Article

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