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《Acta Petrologica Sinica》 2009-10
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Discovery of Xiaogulihe perpotassic basic and ultrabasic volcanic rock in the north-west Heilongjiang province, China

SHAO JiAn~1 , ZHANG WenLan~2 , ZHOU XinHua~3 and ZHANG Cong~1 1.The Key Laboratory of Orogenic Belts and Crusted Evolution, Ministry of Education; School of Earth and Space Sciences Peking University, Beijing 100871, China2.Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Science, Beijing 100029, China3.Department of Earth Sciences, Nanjing University, Nanjing 210093, China  
A suite of basic to urtrabasic per-potassic volcanic rocks in the north part of Wudalianchi rift belt, Heilongjiang province are reported in this paper. On the basin of detailed field investigation, eruption sequence of the volcanic rocks has been identified and was confirmed that they are evolved from basic to urtrabasic with the contant of K_2O and TiO_2 progressively. Such observation leads to a preliminary conclusion about the origin of the ultrabasic- per-potassic rocks, i. e. instead of the resuslt of crystal fractionation of a parental magma, they are produced in an independent typhonic magmatic events against a tectonic background of rift evolution. The Xiaogulihe urtrabasic-perpotassic volcanic rocks were compared with famous potassic volcanic rocks in world as Uganda and Italy etc.
【Fund】: 国家自然科学基金(编号90714008 40672039);; 中国科学院矿产资源研究重点实验室资助项目
【CateGory Index】: P588.1
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