首页> 美国政府科技报告 >Eocene Climates, Depositional Environments, and Geography, Greater Green RiverBasin, Wyoming, Utah, and Colorado: Geology of the Eocene Wasatch, Green River, and Bridger (Washakie) Formations, Greater Green River Basin, Wyoming, Utah and Colorado~Professi
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Eocene Climates, Depositional Environments, and Geography, Greater Green RiverBasin, Wyoming, Utah, and Colorado: Geology of the Eocene Wasatch, Green River, and Bridger (Washakie) Formations, Greater Green River Basin, Wyoming, Utah and Colorado~Professi

机译:始新世气候,沉积环境和地理,大绿河流域,怀俄明州,犹他州和科罗拉多州:始新世瓦萨奇,格林河和布里杰(Washakie)地层,大绿河流域,怀俄明州,犹他州和科罗拉多州〜地区

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The climates, depositional environments, and geography of Eocene rocks in thegreater Green River basin are investigated to determine the origin, mode of deposition, and areal distribution of the Wasatch, Green River, Bridger, and Washakie Formations. The data indicate that Eocene climates ranged from cool temperature to tropical and were affected by both terrestrial and astronomical factors. Eight depositional environments are identified, discussed, and illustrated by diagrams, columnar sections, and photographs. They are: (1) fluvial, (2) paludal, (3) freshwater lacustrine, (4) saltwater lacustrine, (5) pond and laya lake, (6) evaporite (salt pan), (7) mudflat, and (8) volcanic and fluviovolcanic. The areal distribution of the eight depositional environments in the Wasatch, Green River, Bridger, and Washakie Formations is illustrated by photographs and 13 paleographic maps.

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