加拿大新斯科舍省Sable子盆地Penobscot地区侏罗系储层地震反演勘探风险

Qadeer Ahmad
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引用次数: 2

摘要

Penobscot位于加拿大黑貂子盆地的黑貂岛。苏格兰盆地位于北美板块上。这是一个典型的被动非火山共轭边缘。它代表了超过2.5亿年的连续沉积,记录了该地区从最初的大西洋开放到最近的后冰川沉积的动态地质历史。含中生代至新生代的岩性(图1)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mitigation Exploration Risk of Jurassic Reservoir by Seismic Inversion,Penobscot Area, Sable Sub Basin Nova Scotia, Offshore, Canada
Penobscot is located in the Sable Island, Sable sub basin Canada. The Scotian Basin lies on the North American Plate. It is a classic passive, non-volcanic conjugate margin. It represents over 250 million years of continuous sedimentation recording the region’s dynamic geological history from the initial opening of the Atlantic Ocean to the recent post-glacial deposition. It contains the lithology ranging from Mesozoic era to Cenozoic era (Figure 1) [1].
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