RELATIONSHIP BETWEEN SHEAR ZONES AND SR ISOTOPE COMPOSITIONS OF GRANITIC-ROCKS IN THE HIDA BELT, JAPAN

被引:8
作者
ARAKAWA, Y
机构
关键词
D O I
10.1086/629376
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The dextral shear zones in the Hida belt, central Japan, show close temporal and spatial relationships with some of the Late Triassic to Early Jurassic Funatsu granitic intrusions. The Sr isotopic compositions of intrusions associated with the shear zones suggest large crustal contributions to the magma chemistries. In contrast, granitic intrusions not accompanied by shear zones show less crustal signatures. It is suggested that contrasting characteristics in the two types of intrusions reflect different stress conditions. -from Author
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页码:81 / 90
页数:10
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共 61 条
[1]  
[Anonymous], 1980, MEMORIES GEOLOGICAL
[2]  
Arakawa Y., 1984, J JPN ASS MINERAL, V79, P431, DOI [10.2465/ganko1941.79.431, DOI 10.2465/GANKO1941.79.431]
[3]  
ARAKAWA Y, 1982, GEOLOGIC STRUCTURE B, P1
[4]  
ARAKAWA Y, 1989, ANN M GEOL SOC JAPAN, P552
[5]  
Arakawa Y., 1988, J MINERAL PETROL EC, V83, P374
[6]  
Aramaki S., 1972, J GEOLOGICAL SOC JAP, V78, P39
[7]   CRITICAL PHENOMENA IN RHEOLOGY OF PARTIALLY MELTED ROCKS [J].
ARZI, AA .
TECTONOPHYSICS, 1978, 44 (1-4) :173-184
[8]   SOURCE ROCKS OF I-TYPE AND S-TYPE GRANITES IN THE LACHLAN FOLD BELT, SOUTHEASTERN AUSTRALIA [J].
CHAPPELL, BW .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1984, 310 (1514) :693-707
[9]  
CHIHARA K, 1979, 5 NIIG U SCI REPT