论文部分内容阅读
得克萨斯海洋科学协会大学已经完成了在墨西哥海湾大陆斜坡和隆起上记录的两条深水共深度点地震测线的处理。测线布置成等腰三角形的两个边。其顶点约位于北纬27°10′,西经90°10′的北美大陆坡斜上;其边长为150浬;其底东西走向延续距离为100浬。东边的测线与西格斯比崖顶附近的DSDP第92号井相交。西格斯比崖的北部,用4毫秒的取样率记录到了8秒的资料。在崖的南部收集到了16秒的资料
The Texas Ocean University Association has completed the processing of two deep-water total-depth seismic records recorded on the continental slope and uplift of the Gulf of Mexico. The line is arranged in two sides of an isosceles triangle. Its vertex is located at a slope of North American continental slope about 27 ° 10 ’north latitude and 90 ° west longitude 90 °. Its side length is 150 浬 and its east-west distance is 100 浬. The eastern line intersects DSDP No. 92 well near the cliff top of Scutel. In the northern part of Sigusby Cliff, 8 seconds of data was recorded with a sample rate of 4 milliseconds. In the southern cliff collected 16 seconds of information