Condie K C, Kuo C S, Walker R M, Murthy V R
Science. 1969 Jul 4;165(3888):57-9. doi: 10.1126/science.165.3888.57.
Uranium concentrations and distributions in separated clinopyroxenes of eclogites from four different sites have been studied by the fission track method. Types of uranium occurrences included (i) inhomogeneously distributed clusters, (ii) line concentrations at cracks, and (iii) uniform distributions in the body of the mineral. Different grains from the same sample generally vary by factors of 2 to 4 in uniformly distributed uranium concentration. Samples from different locations vary in their average uniformly distributed uranium concentration by a factor of approximately 1000 (that is, from 0.01 to 20 parts per billion of uranium). The degree of homogeneity also varies markedly from one site to the next. The clinopyroxenes from the only oceanic locality studied (Salt Lake Crater) contained both the largest concentration of uranium (15 to 20 parts per billion) and the most uniform uranium distribution. This study suggests that, if total uranium concentrations in eclogitic clinopyroxenes are less than a few parts per billion, much if not most of the uranium may occur as contaminants along cracks or in microinclusions of unknown origin.
利用裂变径迹法研究了来自四个不同地点的榴辉岩中分离出的单斜辉石的铀浓度和分布情况。铀的赋存类型包括:(i)分布不均匀的团簇;(ii)裂缝处的线浓度;(iii)矿物体内的均匀分布。同一样品中的不同颗粒,其均匀分布的铀浓度通常相差2至4倍。不同地点的样品,其平均均匀分布的铀浓度相差约1000倍(即从十亿分之0.01到20)。不同地点的均匀程度也有显著差异。唯一经过研究的大洋地区(盐湖火山口)的单斜辉石,其铀浓度最高(十亿分之15至20),且铀分布最为均匀。这项研究表明,如果榴辉岩中单斜辉石的总铀浓度低于十亿分之几,那么即使不是大部分,也有许多铀可能以污染物的形式存在于裂缝中或来源不明的微包裹体中。