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《Acta Scicentiarum Naturalum Universitis Pekinesis》 2005-04
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Significances of Deep-Seated Xenolith in Cretaceous Basalt of Inner Mongolia

XU Xuan~1),3) WU Tairan~1),3) ZHANG Shuangtao~1),3)J. Byamba~2) A. Amarjargal~2) WANG Shiqi~3) LI Zhongquan 3)( ~1)Key Laboratory of Orogenic Belts and Crustal Evolution (Peking University), Ministry of Education, Beijing, 100871; ~2)Faculty of Earth Science, National University of Mongolia, Ulaanbaatar, Mongolia,210000; ~3) School of Earth and Space Sciences, Peking University, Beijing, 100871)  
Siziwangqi of Inner Mongolia is located on the north margin of North China Craton,the junction of North China Craton and Siberia.Granulite xenoliths are found there in Cretaceous basalt.These xenoliths are mainly plagioclase-pyroxenite.The K-Ar isotopic dating of the basalt is between 108.6-128.4?Ma.These granulite xenoliths are not only important for understanding the composition and interaction between the lower lithosphere and the mantle,but also direct evidence for Mesozoic delamination of North China Craton.
【Fund】: 国家自然科学基金(40072074)资助项目
【CateGory Index】: P548.245
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