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引用次数: 1
摘要
Goshen Hole凸起是Denver Julesburg盆地北端一个鲜为人知且勘探较少的特征，我们认为主要在白垩纪凸起(Hygiene, Niobrara, Wall Creek, Muddy, Dakota)具有良好的油气潜力。侏罗纪(峡谷泉)，二叠纪和宾夕法尼亚目标。在这些层位的地震资料中发现了各种各样的地层异常和大量的古构造。地下室测试大约在10,000至11,000英尺(3.048 - 3.353米)范围内。自宾夕法尼亚纪以来，隆起反复运动;然而，至少在坎帕纪早期开始的上白垩世出现了一段隆升期，并在新生代出现了间歇性隆升。区内古生界和中生界有大量的地下展露和烃源层，隆起处有大量的原油渗漏，提高了该区的开发潜力
The Goshen Hole Uplift: A Brief Review of its History and Exploration Potential
The Goshen Hole uplift 1s a little recognized and sparsely explored feature in the northern end of the Denver Julesburg basin We believe there is excellent hydrocarbon potential on the uplift principally In Cretaceous (Hygiene, Niobrara, Wall Creek, Muddy, Dakota). Jurassic (Canyon Springs), Permian and Pennsylvanian objectives. There are diverse stratigraphic anomalres observed on seismic data in these horizons as well as numerous paleo structures. Basement tests are approximately in the 10.000 to 11,000 ft (3.048 - 3.353 m) range. The uplift has had recurrent movement since the Pennsylvanian; however a period of uplifting occurred in the Upper Cretaceous beginning by at least early Campanian time with intermit- tent uplift rn the Cenozoic. There are numerous subsurface shows and source beds in Paleozoic and Mesozoic horizons and oil seeps on the uplift which enhance the exploitations potential of this area
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