海洋地质前沿2017，Vol.33Issue(8)：1-10,10.DOI:10.16028/j.1009-2722.2017.08001
南海北部边缘壳内低速层发育特征与尖灭成因
CHARACTERISTICS AND PINCH-OUT OF LOW VELOCITY LAYERS IN THE CRUST OF NORTHERN SOUTH CHINA SEA MARGIN
摘要
Abstract
Low Velocity Layer (LVL) zones are commonly seen in South China and the Northern South China Sea (SCS) and pinch out towards the sea basin.It is indispensable to understand the cause of LVL pinch-out in order to disclose the origin and development of the SCS.This article summarized previous studies and compared the distribution of LVL in South China and the Northern SCS based on interpretation of seismic sections from related areas.The results suggest that large fault zones play key roles in LVL pinching out in the Northern SCS.LVL might release its heat along great fault zones,accelerate the process of consolidation of early fusion layer and at the same time make the LVL pinching out.关键词
南海北部边缘/壳内低速层/发育特征/尖灭成因Key words
Northern Margin of South China Sea/low velocity layers/develop characteristics of LVL/pinch-out分类
天文与地球科学引用本文复制引用
黄文凯..南海北部边缘壳内低速层发育特征与尖灭成因[J].海洋地质前沿,2017,33(8):1-10,10.基金项目
海洋地质保障工程资助项目(GZH201100205) （GZH201100205）
