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- W2369936029 abstract "There occur Cenozoic volcanic rocks in Muztag-Cetacean lake area. They are composed mainly of bassltic-andesite, andesite, andesite-basalt and leucite-alkale-basalt. The areas of neutral volcanic rocks are about 99.1 percent. They have the characteristics of calc-alkaline/kali-neutral volcanic rocks. These volcanic rocks are generally rich in LILES (Ba,Rb,K,Sr) and depleted in HFSES (Zr,Hf,Nb).REE distribution patterns are characterized by an enrichment of LREE. The volcanic activities occurred along the giant sinistral strike-slip fault, the deep-cut faults here acted as a magma channel. Isotopic characteristics suggested that these rocks were originated from EMⅡtype of mantle, a kind of REE enriched mantle with the crustal material. New evidence shows that Cenozoic volcanic rocks were formed in a continental extension setting." @default.
- W2369936029 created "2016-06-24" @default.
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- W2369936029 date "2007-01-01" @default.
- W2369936029 modified "2023-09-28" @default.
- W2369936029 title "GEOCHEMICAL CHARACTERISTICS AND TECTONIC SIGNIFICANCE OF CENOZOIC VOLCANIC ROCKS IN MUZTAG-CETACEAN LAKE AREA" @default.
- W2369936029 hasPublicationYear "2007" @default.
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