LOSS OF URANIUM FROM CRYSTALLIZED SILICIC VOLCANIC ROCKS

被引：34

作者：

ROSHOLT, JN

NOBLE, DC

机构：

[1] U.S. Geological Survey, Denver, CO

[2] Department of Geological Sciences, Harvard University, Cambridge, MA

来源：

EARTH AND PLANETARY SCIENCE LETTERS | 1969年 / 6卷 / 04期

关键词：

D O I：

10.1016/0012-821X(69)90166-6

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Dense primarily crystallized silicic groundmass material from two welded ash-flow units and one lava flow of Tertiary age from the Western United States contain only 20 to 60 percent of the uranium present in nonhydrated glass from the rock units. These differences reflect loss of uranium from the crystallized specimens, probably as a result of groundwater leaching. It appears likely that most crystallized silicic volcanic rocks have lost comparable amounts of uranium. © 1969.

引用

页码：268 / &

共 21 条

[1]

[Anonymous], 1968, CONTRIB MINERAL PETR, DOI DOI 10.1007/BF00371729

[2]

CROSS C.W., 1886, AM J SCI, V131, P432

[3] BEARING OF LEAD ISOTOPES ON SOURCE OF GRANITIC MAGMA [J].