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Geology of continental shelf off Point Calimere, Tamil Nadu

机译:泰米尔纳德邦卡利米尔角附近大陆架的地质

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The present work was carried out to understand the morphological features of the seabed through bathymetry, shallow seismic and magnetic surveys off northeast of Point Calimere, Tamil Nadu.The trend of bathymetric contours is in configuration with shoreline alignment, i.e., N-S to NNW-SSE direction. The inner-shelf is demarcated upto 19 m of water depth, the middle-shelf between 19 and 30 m and the outer shelf extends between 25 and 128 m of water depth and zone of continental shelf is so wide that shelf break could not be picked up in the area of study.The shallow seismic survey delineated wedge-shaped sediment in the inner shelf zone. A fault running in NNW-SSE direction around 25 m of isobath acts as divider between middle and outer shelf. In the mid-shelf region a basin-like feature is recorded parallel to coast. The analysis of magnetic data indicates that the area has been traversed by lineaments in different directions. These planes divide the area into several blocks. Depth of magnetic basement varies from 0.5 km to 2.6 km.The sedimentological studies indicate that the seabed sediments are classified into sand, clayey silt and silty sand in order of abundance. The sediments of the inner shelf are terrigenous-dominated and that of outer shelf is relict sand.
机译:目前的工作是通过泰米尔纳德邦卡利米尔角东北方向的测深法,浅层地震和磁测图了解海床的形态特征。测深等高线的趋势是与海岸线对齐,即从NS到NNW-SSE方向。内层架划界至水深达19 m,中层架介于19至30 m之间,而外层架则延伸至水深为25至128 m之间,而大陆架的区域是如此之宽,以至于无法找到层架断裂浅层地震勘测划定了内陆架带的楔形沉积物。在等深线约25 m处沿NNW-SSE方向延伸的断层充当中,外层架的分隔物。在货架中部区域,记录到与海岸平行的盆地状特征。磁数据分析表明该区域已被不同方向上的细纹遍历。这些平面将区域分为几个块。磁性基底的深度从0.5 km到2.6 km不等。沉积学研究表明,海底沉积物按丰度顺序分为砂,黏土粉砂和粉质砂。内层架的沉积物以陆源为主,外层架的沉积物为残砂。

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