| 新疆哈密坡子泉地区首次发现隐爆角砾岩筒 |
| |
| 引用本文： | 白云山,彭湘萍.新疆哈密坡子泉地区首次发现隐爆角砾岩筒[J].新疆地质,1999(2). |
| |
| 作者姓名： | 白云山 彭湘萍 |
| |
| 作者单位： | 新疆地质矿产勘查开发局第一区域地质调查大队 |
| |
| 摘 要： | 新疆哈密坡子泉地区首次发现的隐爆角砾岩筒处在塔里木板块北缘活动带卡瓦布拉克微板块之上，基底地层为前寒武系，盖层主要为石炭系，受ＮＥ向断裂带控制。隐爆角砾岩特征及产出环境相似于金伯利岩。
|
| 关 键 词： | 哈密 坡子泉 石炭系 隐爆角砾岩 |
DISCOVERY OF CRYPLOEXPLOSIVE BRECCIA CHIMNEY IN PUOZIQUAN AREA OF HAMI,XINJIANG |
| |
| BAI Yun shan,PENG Xiang ping.DISCOVERY OF CRYPLOEXPLOSIVE BRECCIA CHIMNEY IN PUOZIQUAN AREA OF HAMI,XINJIANG[J].Xinjiang Geology,1999(2). |
| |
| Authors: | BAI Yun shan PENG Xiang ping |
| |
| Abstract: | The cryptoexplosive breccia chimney first discovereed in Puoziquan area is produced on the Kawabulak micro block of north margional active belt of Tarim plate.the basement is pre Cambrian and the cover is Carboniferous.It is controlled by the northeast fault belt and its petrological characteristics and foming environment are similar to kimberlite |
| |
| Keywords: | Xinjiang Hami Puoziquan Carboniferous cryptoexplosive breccia chimney |
| 本文献已被 CNKI 等数据库收录！ |
