| 车步单元地质特征及时代初探 |
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| 引用本文： | 吴旭玲,欧阳克贵.车步单元地质特征及时代初探[J].华东地质学院学报,2000,23(2):121-123. |
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| 作者姓名： | 吴旭玲 欧阳克贵 |
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| 作者单位： | 江西地质调查院，江西南昌县330201 |
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| 摘 要： | 车步单元为基性侵入体，同于钛铁矿含量较高，发现有多处矿点，与成密切相关，在岩石化学特征及成岩时代上与区域菖蒲组玄武岩有同期同源性，定位时代为早侏罗世。
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| 关 键 词： | 早侏罗世 车步单元 基性侵入体 侵位年代 成矿作用 |
| 文章编号： | 1000-2251(2000)02-121-03 |
| 修稿时间： | 1999年11月27 |
The Conceptual Inquisition of Geological Character and Location Era in Chebu Unitr |
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| WU Xuling,OU YANG kegui.The Conceptual Inquisition of Geological Character and Location Era in Chebu Unitr[J].Journal of East China Geological Institute,2000,23(2):121-123. |
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| Authors: | WU Xuling OU YANG kegui |
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| Abstract: | Chebu unit is basic instrusive body. As the content of ilmenite is ligh, if finds that there are many gritpointsconnects with shaped mine closely. The chemical character and shaped mine period of the rock and basalt in chang pugroup district have synchronism and homogeneous. The oviented period is early Jurasic Period. |
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| Keywords: | Early Jurassic Period Unit Location Period chebu unit Jiangxi Dingnan |
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