Rare Earths of Two Types Granites in Sawuer Region, Xinjiang
来源期刊：JOURNAL OF RARE EARTHS2005年第5期
论文作者：Zhou Taofa Yue Shucang Fan Yu Tan Lugui Yuan Feng
Key words：granite; post-collisional; Sawuer region; Xinjiang; rare earths;
Abstract: The geochemical characteristics of rare earth elements of A type and I type granites were studied in the Sawuer region, Xinjiang. The characteristics of two types granites are different obviously,because the A type and I type granites formed at different stage of the post-collisional period. The Sentasi intrusion and Wokensala intrusion are the I type granites formed at the late of post-collisional period, and there is extrusion translating to extension stress. The characteristics of rare earth elements show that the fractional crystallization of the I type granites is indistinct, and the sources of the I type granites come from the mantle. The Kuoyitasi intrusion and Qiaqihai intrusion are the A type granites formed at the end of post-collisional period, and there is extension stress. The characteristics of rare earth elements show that the fractional crystallization of the A type granites is distinct. The sources of the A type granites come from the mantle but interfused by the crust.
Zhou Taofa1，Yue Shucang1，Fan Yu1，Tan Lugui1，Yuan Feng1
(1.School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China)
Abstract:The geochemical characteristics of rare earth elements of A type and I type granites were studied in the Sawuer region, Xinjiang. The characteristics of two types granites are different obviously,because the A type and I type granites formed at different stage of the post-collisional period. The Sentasi intrusion and Wokensala intrusion are the I type granites formed at the late of post-collisional period, and there is extrusion translating to extension stress. The characteristics of rare earth elements show that the fractional crystallization of the I type granites is indistinct, and the sources of the I type granites come from the mantle. The Kuoyitasi intrusion and Qiaqihai intrusion are the A type granites formed at the end of post-collisional period, and there is extension stress. The characteristics of rare earth elements show that the fractional crystallization of the A type granites is distinct. The sources of the A type granites come from the mantle but interfused by the crust.
Key words:granite; post-collisional; Sawuer region; Xinjiang; rare earths;
【全文内容正在添加中】
