{"title":"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","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":"{\"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}","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}
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].