{"title":"乔治滩COST G-2井生物地层学:晚三叠世共融蒸发岩沉积记录里阿斯统的凸起;中侏罗统至中新世海相沉积","authors":"H. Cousminer, W. Steinkraus","doi":"10.1016/B978-0-444-42903-2.50012-9","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":122711,"journal":{"name":"Developments in Geotectonics","volume":"35 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"13","resultStr":"{\"title\":\"Biostratigraphy of the COST G-2 well (Georges Bank): a record of Late Triassic synrift evaporite deposition; Liassic doming; and mid-Jurassic to Miocene postrift marine sedimentation\",\"authors\":\"H. Cousminer, W. Steinkraus\",\"doi\":\"10.1016/B978-0-444-42903-2.50012-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":122711,\"journal\":{\"name\":\"Developments in Geotectonics\",\"volume\":\"35 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"13\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Developments in Geotectonics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1016/B978-0-444-42903-2.50012-9\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Developments in Geotectonics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1016/B978-0-444-42903-2.50012-9","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Biostratigraphy of the COST G-2 well (Georges Bank): a record of Late Triassic synrift evaporite deposition; Liassic doming; and mid-Jurassic to Miocene postrift marine sedimentation