| 埕岛地区构造体系归属探讨 |
| |
| 引用本文： | 陈广军,隋风贵.埕岛地区构造体系归属探讨[J].大地构造与成矿学,2001,25(4):405-411. |
| |
| 作者姓名： | 陈广军 隋风贵 |
| |
| 作者单位： | 胜利油田有限公司地质院, |
| |
| 摘 要： | 埕岛地区是一个异常复杂的潜山披覆构造带，已取得了很大的勘探成果，但它在区域构造中的位置和关系一宜不太清楚，影响到进一步的勘探。该文从构造演化、沉积发育等方面分析了埕岛地区的地层、构造及沉积特征，说明桩西潜山和埕岛潜山地质历史时期曾经属于同一构造带；埕岛构造应该属于沾化凹陷构造体系，而非以前那样即把它划在沾化体系之外，又不能够确定它属于渤中构造体系，从而对该区的勘探研究起到较大的促进作用。
|
| 关 键 词： | 埕岛地区 潜山披覆构造 沾化凹陷 渤中凹陷 构造运动 沉积中心 |
| 文章编号： | 1001-1552(2001)04-405-07 |
| 修稿时间： | 2001年6月25日 |
DISCUSSION ON WHICH TECTONIC SYSTEM DOES CHENGDAO BELONG TO |
| |
| Abstract: | The Chengdao region is one very complicated buried hill zone, now many progresses have been made. But it is not clear that the region belongs to which system and how to relate to others, and this has affected the next exploration. This paper analyses the strata, structure and the characters of deposition in Chengdao, shows the buried hill of Chengdao and Zhuangxi has belonged to one zone in geological history. The structure of Chengdao should be in the Zhanhua structure system, not like the old opinion that not only regarding it as out Zhanhua system, but also not determining it belongs to Bozhong system, which promotes the study on exploration in this area. |
| |
| Keywords: | Chengdao area buried hill Zhanhua depression Bozhong depression tectonic movement deposition centre |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
