首页> 美国政府科技报告 >Fracture History of the Divide Creek and Wolf Creek Anticlines and Its Relationto Laramide Basin-Margin Tectonism, Southern Piceance Basin, Northwestern Colorado (Chapter Z)
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Fracture History of the Divide Creek and Wolf Creek Anticlines and Its Relationto Laramide Basin-Margin Tectonism, Southern Piceance Basin, Northwestern Colorado (Chapter Z)

机译:分裂河和狼溪背斜的断裂历史及其与拉腊德盆地边缘构造作用的关系,南部piceance盆地,科罗拉多州西北部(Z章)

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The Divide Creek and Wolf Creek anticlines are two gentle, north-northwest-trending, gas-producing intrabasin folds near the eastern margin of the Piceance basin of northwestern Colorado. Both folds developed above a decollement on the basinward side of a large, basement-involved thrust wedge that resulted from

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