Dating of Igneous Dike, Eastern Uinta Mountains

Utah Geology Pub Date : 1900-01-01 DOI:10.34191/ug-1-1_95
H. Ritzma
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Abstract

Age of a gabbroic dike which intrudes the Precambrian metasediments of the Uinta Mountains in T. 1 S., Rs. 18 and 19 E. , Uintah County, Utah, has been determined by the K-Ar method. Analyses of the whole rock and a feldspar concentrate from it were run. The whole-rock determination gave an age of 412 ± 17 my and the feldspar concentrate 453 ± 17 my. The whole-rock determination would place the age in the uppermost Silurian; the feldspar concentrate determination would place the age as medial to uppermost Ordovician. Geochron Laboratories Division of Krueger Enterprises, Inc., Cambridge, Massachusetts, who performed the analyses, commented that this rock is at least lower Paleozoic in age, and almost certainly it is pre-Devonian.
东温塔山脉火成岩岩脉的年代测定
用K-Ar法测定了犹他州犹他县T. 1 S、r . 18和r . 19 E.犹他山脉前寒武纪变质沉积层中的一条辉长岩岩脉的年龄。对整块岩石和其中的长石精矿进行了分析。全岩测定年龄为412±17岁,长石精矿年龄为453±17岁。全岩测定将其年龄定在志留纪上端;长石精矿测定表明其年龄为奥陶系中上段。马萨诸塞州剑桥市克鲁格企业公司的地质年代实验室部门进行了分析,他们评论说,这块岩石的年龄至少是下古生代,几乎可以肯定它是前泥盆纪。
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