{"title":"Mitigation Exploration Risk of Jurassic Reservoir by Seismic Inversion,Penobscot Area, Sable Sub Basin Nova Scotia, Offshore, Canada","authors":"Qadeer Ahmad","doi":"10.4172/2329-6755.1000123","DOIUrl":null,"url":null,"abstract":"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].","PeriodicalId":344421,"journal":{"name":"Journal of Geology and Geosciences","volume":"87 1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-07-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geology and Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4172/2329-6755.1000123","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
Abstract
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].