犹他州比弗县恒星范围的详细磁测量

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-1-1_51
J. Schmoker
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引用次数: 0

摘要

在星域的四个区域获得了垂直场地磁数据,并根据成因地质构造进行了解释。对Milford Flat侵入体进行了8条磁剖面研究,为解释冲积层下的侵入构造提供了依据。在野比尔矿附近获得了栅格磁数据。在这些资料中没有明显的大面积接触矿化带;格网中南部的异常是由于局部侵入体向上突出所致。沿着shaute侵入体的东南接触面,磁数据显示有四个明显的磁铁矿矿化区,厚度从8英尺到25英尺不等。在暴露的shaute侵入岩南部收集的数据显示了一个起源不确定的异常,可能反映了东南接触带的埋藏。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Detailed Magnetic Surveys in the Star Range, Beaver County, Utah
Vertical-field ground magnetic data were obtained in four areas of the Star Range, and interpreted in terms of causative geologic structures. Eight magnetic profiles were taken over the Milford Flat intrusive body, and provided the basis for interpreting the intrusive structure under the alluvium. Gridded magnetic data were obtained in the vicinity of the Wild Bill mine. No extensive zones of contact mineralization are apparent in this data; an anomaly in the south-central portion of the grid is attributed to an upward protrusion of the local intrusive body. Along the southeastern contact of the Shauntie intrusive body, magnetic data show four areas of appreciable magnetite mineralization ranging from eight to twenty-five feet thick. Data collected south of the exposed Shauntie intrusive show an anomaly of uncertain origin that probably reflects the buried southeastern contact zone.
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