{"title":"Quealy Dome, Albany County, Wyoming:落基山脉前陆构造圈闭油田","authors":"D. L. Blackstone","doi":"10.31582/rmag.mg.21.3.85","DOIUrl":null,"url":null,"abstract":"Quealy Dome, Albany County, Wyoming, is an asymmetric Rocky Mountain foreland fold on the west flank of the Laramie basin. Production is from the Lower Cretaceous Muddy Sandstone and Dakota Sandstone and from the Jurassic Sundance Formation and Permian-Pennsylvanian Casper Formation. Accumulation is structurally controlled. Internal structure of the fold involves \"out-of-the-syncline\" thrusting and post-folding normal faulting.","PeriodicalId":101513,"journal":{"name":"Mountain Geologist","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"1984-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Quealy Dome, Albany County, Wyoming: A Rocky Mountain Foreland Structural Trap Oil Field\",\"authors\":\"D. L. Blackstone\",\"doi\":\"10.31582/rmag.mg.21.3.85\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Quealy Dome, Albany County, Wyoming, is an asymmetric Rocky Mountain foreland fold on the west flank of the Laramie basin. Production is from the Lower Cretaceous Muddy Sandstone and Dakota Sandstone and from the Jurassic Sundance Formation and Permian-Pennsylvanian Casper Formation. Accumulation is structurally controlled. Internal structure of the fold involves \\\"out-of-the-syncline\\\" thrusting and post-folding normal faulting.\",\"PeriodicalId\":101513,\"journal\":{\"name\":\"Mountain Geologist\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1984-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mountain Geologist\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.31582/rmag.mg.21.3.85\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mountain Geologist","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31582/rmag.mg.21.3.85","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Quealy Dome, Albany County, Wyoming: A Rocky Mountain Foreland Structural Trap Oil Field
Quealy Dome, Albany County, Wyoming, is an asymmetric Rocky Mountain foreland fold on the west flank of the Laramie basin. Production is from the Lower Cretaceous Muddy Sandstone and Dakota Sandstone and from the Jurassic Sundance Formation and Permian-Pennsylvanian Casper Formation. Accumulation is structurally controlled. Internal structure of the fold involves "out-of-the-syncline" thrusting and post-folding normal faulting.