犹他州Juab和Millard县富玛孔丘地区的重力研究

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-5-1_37
T. Smith, K. Cook, W. J. Peeples
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引用次数: 3

摘要

1973年对福玛罗比特地区进行了重力调查,包括位于犹他州三角洲西北约39公里(22英里)处的火山口泉KGRA(贝克温泉)。大约有500个站点作为地热勘探技术研究的一部分。调查区域包括Juab和Millard县的部分地区,以及沙漠、麦克道尔和德拉姆山脉的部分地区。计算了简单的布格重力异常图,并建立了两条东西向重力剖面的二维地质模型。对重力数据的分析,结合已知的地质学和其他地球物理研究的结果,得出了以下解释:1)表明存在两个埋藏的侵入体——一个是位于贝克温泉和富玛孔巴特熔岩流东部边缘的北-北-西向岩脉,另一个位于沙漠山西南几英里处;2)圈定了先前未发表的盆地和山脉断裂及相关地堑;3)基底弯曲带假定的裂缝的存在,这些裂缝充当了上涌岩浆到达富玛孔巴特表面的管道。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Gravity Study of the Fumarole Butte Area, Juab and Millard Counties, Utah
A gravity survey was made in 1973 of the Fumarole Butte area, including the Crater Springs KGRA (Baker Hot Springs), located approximately 39 km (22 miles) NW of Delta, Utah. About 500 stations were taken as part of a study of geothermal exploration techniques. The region of investigation includes portions of both Juab and Millard Counties and incorporates parts of the Desert, McDowell and Drum Mountains. A simple Bouguer gravity anomaly map was computed and two-dimensional geologic models were prepared for two east-west gravity profiles. The analysis of the gravity data, in conjunction with the known geology and the results from other geophysical studies, led to the following interpretations: 1) the indication of two buried intrusive bodies - one a north north westward-trending dike lying beneath the Baker Hot Springs and the eastern margin of the Fumarole Butte lava flows and another several miles southwest of Desert Mountain; 2) the delineation of previously ' unpublished Basin and Range faults and associated grabens; and 3) the existence of a basement flexure with postulated fractures that served as conduits for the upwelling magma to reach the surface at Fumarole Butte.
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