THERMOCHRONOLOGIC EVIDENCE OF MAJOR TECTONIC DENUDATION ASSOCIATED WITH DETACHMENT FAULTING, NORTHERN RUBY MOUNTAINS - EAST HUMBOLDT RANGE, NEVADA

被引:92
作者
DOKKA, RK [1 ]
MAHAFFIE, MJ [1 ]
SNOKE, AW [1 ]
机构
[1] UNIV WYOMING,DEPT GEOL & GEOPHYS,LARAMIE,WY 82071
关键词
D O I
10.1029/TC005i007p00995
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
引用
收藏
页码:995 / 1006
页数:12
相关论文
共 46 条
[1]  
ALLMENDINGER RW, 1983, GEOLOGY, V11, P532, DOI 10.1130/0091-7613(1983)11<532:CAMSOT>2.0.CO
[2]  
2
[3]  
ANDERSON RE, 1971, GEOL SOC AM BULL, V82, P43, DOI 10.1130/0016-7606(1971)82[43:TSDITR]2.0.CO
[4]  
2
[6]  
BLACKWELL DD, 1985, P VOLUME C HEAT DETA, P12
[7]  
BLACKWELL DD, 1984, GEOL SOC AM ABSTR, V16, P446
[8]  
CARPENTER SB, 1974, NBS26049 SPEC PUBL
[9]   THE MESOZOIC-CENOZOIC TECTONOTHERMAL EVOLUTION OF THE RUBY MOUNTAINS, EAST HUMBOLDT RANGE, NEVADA - A CORDILLERAN METAMORPHIC CORE COMPLEX [J].
DALLMEYER, RD ;
SNOKE, AW ;
MCKEE, EH .
TECTONICS, 1986, 5 (06) :931-+
[10]  
DAVIS GH, 1979, GEOLOGY, V7, P120, DOI 10.1130/0091-7613(1979)7<120:GDOTCM>2.0.CO