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印度孟买岸外西部陆架淹没沙脊——晚更新世—全新世海平面变化的证据ＷａｇｌｅＢ．Ｇ等１．背景研究区位于印度西部陆架１７°２０′Ｎ—１９°３０′Ｎ范围内，这里的陆架宽度＞３００ｋｍ，坡折出现在水深８０—１２５ｍ之间，地形上，内陆架以平坦地形为特征，微向西...
Submerged Sand Ridge on the Western Shore of Mumbai, India - Late Pleistocene - Evidence from Holocene Sea Level Changes. G et al. Background The study area is located within the range of 17 ° 20’N-19 ° 30’N on the shelf of West India, where the shelf width is> 300 km and the slope break occurs between 80 and 125 m. The topography and the inland shelf are characterized by a flat topography , Micro-west ...