辽东半岛东南部潮沙脊特征及其影响因素:辽东半岛东南部潮沙脊特征及其影响因素

Xiaohui Chen, Xun-hua Zhang, Ri-hui Li, Xianhong Lan
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引用次数: 2

摘要

利用高分辨率地震剖面和前人的研究成果,对辽东半岛东南部近海潮汐沉积体系特征进行了研究。结果表明,潮砂脊在地震剖面上表现为不对称丘状和斜前积反射构型,顶部为活动沙波,表明潮砂脊是由侵蚀作用或侵蚀堆积作用形成的,目前仍处于活动状态。研究区内有4条NE-SW平行分布的潮砂脊,其走向与M2组成椭圆的长、短轴线一致。潮沙脊长35~75 km,高3~17 m,宽3~7 km,分布在水深40 ~ 50 m。潮砂脊的沉积特征受研究区潮汐特征和海平面变化的影响。砂脊的物源是多元的,既有经过老铁山海峡的退潮侵蚀物,也有沿海岛屿及邻近地区的侵蚀物,还有河流输入物和海岸流的碎屑。
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CHARACTERISTICS OF TIDAL SAND RIDGES OFF THE SOUTHEAST LIAODONG PENINSULA AND INFLUENCE FACTORS: CHARACTERISTICS OF TIDAL SAND RIDGES OFF THE SOUTHEAST LIAODONG PENINSULA AND INFLUENCE FACTORS
High resolution seismic profiles and previous research progresses have been used to study the characteristics of the tidal depositional system off the coastal area of southeast Liaodong Peninsula.The results indicate that the tidal sand ridges show asymmetrical-mound and oblique progradational reflection configuration on the seismic profiles,topped by active sand waves,suggesting that they are formed by erosion or by erosion and accumulation and still active.There are four NE—SW distributed tidal sand ridges parallel to each other in the study area,whose orientation is agree with the major and minor axes of the ellipses of M2 constituent.The tidal sand ridges are 35~75 km long and 3~17 m high,3~7 km wide distributed in a water depth of 40 to 50 m.The sedimentary characteristics of the tidal sand ridges are influenced by the characters of tide and the change in sea level in the study area.The provenance of the sand ridges is multiple,which includes the eroded matters from the ebb current through the Laotieshan Channel,eroded matters from coastal island and neighborhood,river inputs and detritus from coastal currents.
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