OXYGEN ISOTOPE EVIDENCE FOR LARGE-SCALE INTERACTION BETWEEN METEORIC GROUND WATERS AND TERTIARY GRANODIORITE INTRUSIONS, WESTERN CASCADE RANGE, OREGON

被引:180
作者
TAYLOR, HP
机构
来源
JOURNAL OF GEOPHYSICAL RESEARCH | 1971年 / 76卷 / 32期
关键词
D O I
10.1029/JB076i032p07855
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
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页码:7855 / &
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共 20 条
[1]  
[Anonymous], 1968, CONTRIB MINERAL PETR, DOI DOI 10.1007/BF00371729
[2]  
Buddington AF, 1936, AM J SCI, V31, P421
[3]  
CALLAGHAN E, 1938, 893 US GEOL SURV B
[4]   ISOTOPIC VARIATIONS IN METEORIC WATERS [J].
CRAIG, H .
SCIENCE, 1961, 133 (346) :1702-&
[5]   VARIATION OF O-18 CONTENT OF WATERS FROM NATURAL SOURCES [J].
EPSTEIN, S ;
MAYEDA, T .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1953, 4 (05) :213-224
[6]   THE VARIATION OF THE DEUTERIUM CONTENT OF NATURAL WATERS IN THE HYDROLOGIC CYCLE [J].
FRIEDMAN, I ;
REDFIELD, AC ;
SCHOEN, B ;
HARRIS, J .
REVIEWS OF GEOPHYSICS, 1964, 2 (01) :177-224
[7]   THE COOLING OF IRREGULARLY SHAPED IGNEOUS BODIES [J].
JAEGER, JC .
AMERICAN JOURNAL OF SCIENCE, 1961, 259 (10) :721-734
[8]  
LUTTON RJ, 1962, THESIS U ARIZONA
[9]  
ONEIL JR, 1967, AM MINERAL, V52, P1414
[10]  
PECK DL, 1964, 449 US GEOL SURV PRO