Cave Gulch 3-D Survey, Wind River Basin, Wyoming: A major gas discovery developed using poststack depth migration

Autor:	Fred Barrett, Peter Dea, Roy Roux, Steven G. Natali
Rok vydání:	2000
Předmět:	Frontier geography Paleontology Geophysics geography.geographical_feature_category Cave Gulch Drainage basin Geology Arch Geomorphology
Zdroj:	The Leading Edge. 19:1286-1294
ISSN:	1938-3789 1070-485X
DOI:	10.1190/1.1438524
Popis:	Waltman Arch, a transbasinal arch that trends northward across the Wind River Basin of central Wyoming, is overridden by the Owl Creek Thrust at its northern terminus (Figures 1 and 2). Fields along Waltman Arch produce from multiple stacked sandstone pays in the Fort Union, Lance, Meeteetse, Mesa Verde, Frontier, Muddy, and Lakota Formations (Figures 3 and 4). To the northwest, in Madden Field, there is excellent production from deeper Madison carbonates.
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ab117ca5ea0f56ffd892556b13464300 https://doi.org/10.1190/1.1438524 Zobrazit plný text záznamu