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| 台湾峡谷中段沉积特征及流体机制探讨 | |
| 引用本文： | 徐尚,王英民,彭学超,杨彩虹,李华,曹健志,郑贵春,赵亚楠.台湾峡谷中段沉积特征及流体机制探讨[J].地质论评,2013,59(5):845-852. |
| 作者姓名： | 徐尚 王英民 彭学超 杨彩虹 李华 曹健志 郑贵春 赵亚楠 |
| 作者单位： | 1. 中国石油大学(北京)地球科学学院,北京,102249 2. 国土资源部广州海洋地质调查局,广州,510760 3. 中国石油化工股份有限公司上海油气分公司,上海,200120 4. 中化石油勘探开发有限公司,北京,100031 |
| 基金项目： | 本文为国家自然科学基金资助项目（编号 40972077）的成果。 |
| 摘 要： | 海底峡谷、高弯度水道等深水沉积单元中的流体活动方式是人们关注的热点.本次研究利用高分辨地震资料,结合地形地貌特征对台湾峡谷中段的沉积特征及流体活动方式进行初步探讨.台湾峡谷中段发育内堤岸(inner levee),它成层性好、地层产状倾斜,地震反射特征与峡谷西岸和下覆滑塌体明显不同,内部结构表现为逐级上超的特征,以侧向加积为主.曲流河和深水高弯度水道的点坝均发育于河(水)道拐弯处,由于离心力作用,沉积物在凸岸堆积形成点坝.该内堤岸位于峡谷中段直线型地段,不具备形成点坝的地形地貌条件,综合分析认为该内堤岸是由垂直于峡谷轴向、自西向东的底流与沿峡谷向下的重力流交互作用形成的. |
| 关 键 词： | 内堤岸 重力流 底流 交互作用 流体机制 台湾峡谷 |
| 收稿时间： | 2012/12/24 0:00:00 |
| 修稿时间： | 2013/6/14 0:00:00 |
Sedimentary Characteristics and Fluid Mechanism in the Middle Segment of the Taiwan Canyon |
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| Institution: | College of Geosciences, China University of Petroleum, Beijing, 102249;College of Geosciences, China University of Petroleum, Beijing, 102249;Guangzhou Marine Geological Survey Bureau, Guangzhou, 510760;Shanghai Offshore Petroleum Branch, SINOPEC, Shanghai, 200120;College of Geosciences, China University of Petroleum, Beijing, 102249;Petroleum Exploration & Production Co., Ltd., SINOCHEM, Beijing, 100031;College of Geosciences, China University of Petroleum, Beijing, 102249;College of Geosciences, China University of Petroleum, Beijing, 102249 |
| Abstract: | Fluid activity in the deep water sedimentary unit of the high sinuous submarine channels, submarine canyons are the focus nowadays. This study uses high resolution seismic data, combined with the geomorphologic features to discuss the sedimentary characteristics and fluid mechanism in the middle segment of the Taiwan Canyon. There is an inner levee located in the middle Taiwan Canyon. The internal structure of this inner levee is characterized by obviously onlap and lateral accretion. In meandering rivers and high sinuous submarine channels, due to the change of geomorphologic or the decrease of slope, the sediment started to unload. When it went through the bend, with the action of centrifugal force, massive sediment accumulated at the convex bank. Non similar with the rivers and high sinuous submarine channels, the inner levee is located in the straight segment of the middle canyon, where has no geomorphologic condition to form the point bars. The inner levee can be interpreted as the product of interaction between down and along slope processes. |
| Keywords: | inner levee gravity current bottom current interaction fluid mechanism Taiwan Canyon |
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