| 天津空港牡蛎礁:中全新世环境恶化与新构造控礁作用 |
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| 引用本文： | 王海峰,王 宏,范昌福,方 晶,裴艳东,方念乔.天津空港牡蛎礁:中全新世环境恶化与新构造控礁作用[J].地质通报,2012,31(9):1387-1393. |
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| 作者姓名： | 王海峰 王 宏 范昌福 方 晶 裴艳东 方念乔 |
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| 作者单位： | 1. 广州海洋地质调查局,广东 广州 510075; 2. 中国地质调查局天津地质调查中心,天津 300170;
3. 中国地质大学(北京)海洋学院,北京 100083; 4. 中国地质科学院矿产资源研究所,北京 100037;
5. 天津师范大学城市与环境科学学院, 天津 300387 |
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| 基金项目： | 国家自然科学基金面上项目《渤海湾西北岸埋藏牡蛎礁古环境重建》(批准号:40872106);中国地质调查局项目《中国泥质海岸带对全球变化响应的研究与趋势预测》(编号:1212010911069);天津古海岸与湿地国家级自然保护区处项目《贝壳堤、牡蛎礁新发现与新问题研究》 |
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| 摘 要： | 新发现的天津空港埋藏牡蛎礁体和下伏、上覆泥层的沉积学、AMS14C年代学研究显示,厚2.3m的礁体分为3部分,起讫年龄是6170～3980cal BP。5900～4100cal BP的中部,是受全新世冷事件4环境恶化控制的缓慢发育期。礁体的结束,则与冷事件3在时间上大致吻合。根据新的年龄数据,将该礁体的归属重新厘定为Ⅲ-2礁群。探讨礁体主要发育区与新构造活动的关系,表明全新世牡蛎礁平原主要位于海河-宝坻-工部-蓟运河断裂圈闭的北西-南东向区域内。这一认识,进一步从实证角度证实了牡蛎礁形成于渤海湾"湾中之湾"的推测。
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| 关 键 词： | 埋藏牡蛎礁 年代测定 环境恶化 新构造运动 |
Konggang oyster reef in Tianjin constrained by both the Mid-Holocene environmental deteriorations and the local neotectonic faults |
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| WANG Hai-feng,WANG Hong,FAN Chang-fu,FANG Jing,PEI Yan-dong,FANG Nian-qiao.Konggang oyster reef in Tianjin constrained by both the Mid-Holocene environmental deteriorations and the local neotectonic faults[J].Geologcal Bulletin OF China,2012,31(9):1387-1393. |
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| Authors: | WANG Hai-feng WANG Hong FAN Chang-fu FANG Jing PEI Yan-dong FANG Nian-qiao |
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| Institution: | 1. Guangzhou Marine Geological Survey, Guangzhou 510075, Guangdong, China;
2. Tianjin Center of China Geological Survey (CGS), Tianjin 300170, China;
3. School of Marine Sciences, China University of Geosciences, Beijing 100083, China;
4. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;
5. College of Urban and Environmental Science,Tianjin Normal University, Tianjin 300387, China |
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| Abstract: | The buried Konggang oyster reef, located in the northwestern coast of Bohai Bay, is a newly observed reef. Systematical sampling was carried out in the reef body and the underlying and overlying muddy sediments, respectively. AMS 14C dating shows that the duration of this reef is about 2200a from 6170 to 3980cal BP. The reef, 2.3 m thick, can be divided into three parts. Its middle part, 5900-4100cal BP, is a slowly-developed stagnant period coinciding with Cold Event 4. The end of the reef development was approximately consistent with Cold event 3. According to the new AMS 14C data, the reef has been reassigned to oyster reef Group III-2. Based on scrutinizing the relationship between the oyster reef development and the neotectonic movement, the authors hold that the Holocene oyster reef plain is mainly constrained by the alignment of Haihe-Baodi-Gongbu-Jiyunhe faults. This recognition has further proved the presumption that the oyster reefs were spatially distributed mainly in the so-called "Inner Bay" of the Bohai Bay. |
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| Keywords: | buried oyster reef age dating environmental deterioration neotectonic movement |
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