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首页> 外文期刊>The Mountain Geologist >Greater Natural Buttes Field, Uirsta Basin, Utah1
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Greater Natural Buttes Field, Uirsta Basin, Utah1

机译:犹他州Uirsta盆地更大的天然小山场1

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摘要

The Greater Natural Buttes Field (GNB) is a continuous natural gas accumulation producing from tight sandstones located in the northeast part of the Uinta Basin of northeastern Utah. The Uinta is an asymmetrical basin with a west-northwest trending axis and steepest limb to the north, which ultimately culminates into the Uinta Uplift. The basin is bounded by the Uncompahgre Uplift on the southeast, the San Rafael Swell on the southwest, and Charleston Overthrust segment of the Sevier Orogenic Belt on the west, and is separated from the Piceance Basin to the east by the Douglas Creek Arch (Fig. 1).
机译:大天然小山田(GNB)是连续的天然气成藏,它由位于犹他州东北部Uinta盆地东北部的致密砂岩产生。乌因塔(Uinta)是一个不对称盆地,具有西北偏西的趋向轴,向北倾斜的肢体最陡,最终达到乌因塔隆起。该盆地以东南部的Uncompahgre隆起,西南部的San Rafael隆​​起和西部的Sevier造山带的查尔斯顿Overthrust段为界,并被道格拉斯溪拱道与东从Piceance盆地隔开(图1)。

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