首页> 外文期刊>Marine and Petroleum Geology >Morphology of pockmarks along the western continental margin of India: Employing multibeam bathymetry and backscatter data
【24h】

Morphology of pockmarks along the western continental margin of India: Employing multibeam bathymetry and backscatter data

机译:印度西部大陆边缘的麻状形态:利用多光束测深和反向散射数据

获取原文
获取原文并翻译 | 示例
           

摘要

This study addresses the morphology of pockmarks along the western continental margin of India using multibeam bathymetry and backscatter data. Here, for the first time we have utilized the application of ArcGIS (Geographical Information System) for understanding the morphology of pockmarks from the western continental margin of India. The pockmarks observed in water depths of 145-330 m are circular, elliptical or elongated in plan-view, with an average length and width of 157 (±72) m and 83 (±19) m respectively. The average pockmark relief and perimeter are 1.9 (±0.9) m and 412 (±181) m, respectively. The pockmarks have average areas and volumes of 10 759 m2 and 15 315 m~3 respectively. Spatial separation that coincides with 210 m isobath divides the pockmarks into two groups with differing distributions and morphologies. These pockmarks originated from seepages of biogenic or thermogenic gas or from pore fluids from deeper sources, migrated vertically along the faults. Besides a possible structural control, the pockmark morphologies are also affected by bottom currents and/or by submarine slumping. The average acoustic backscatter strength from pockmark centre is higher (-35 dB) than the average backscatter of the total area (-40 dB), which suggests their possible linkage to the precipitation of diagenitic minerals from biodegradation of seepage material.
机译:这项研究使用多光束测深法和反向散射数据处理了印度西部大陆边缘的麻子形态。在这里,我们首次利用ArcGIS(地理信息系统)的应用程序来了解印度西部大陆边缘的麻子形态。在145-330 m的水深中观察到的麻点在平面图中为圆形,椭圆形或细长形,平均长度和宽度分别为157(±72)m和83(±19)m。平均麻纹浮雕和周长分别为1.9(±0.9)m和412(±181)m。麻点的平均面积和体积分别为10 759 m2和15 315 m〜3。与210 m等压线相吻合的空间分隔将麻点分为具有不同分布和形态的两组。这些麻点源自生物气或热气的渗漏,或者来自深层气孔流体,沿着断层垂直迁移。除了可能的结构控制外,麻点形貌还受到底流和/或海底塌陷的影响。麻点中心的平均声反向散射强度(-35 dB)比总面积的平均反向散射强度(-40 dB)高,这表明它们可能与渗流材料生物降解引起的洋生辉石矿物沉淀有关。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号