FLOW STRENGTHS OF QUARTZ AGGREGATES - GRAIN-SIZE AND PRESSURE EFFECTS DUE TO HYDROLYTIC WEAKENING

被引：244

作者：

KRONENBERG, AK ^{[1
]}

TULLIS, J ^{[1
]}

机构：

[1] BROWN UNIV,DEPT GEOL SCI,PROVIDENCE,RI 02912

来源：

JOURNAL OF GEOPHYSICAL RESEARCH | 1984年 / 89卷 / NB6期

关键词：

D O I：

10.1029/JB089iB06p04281

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

页码：4281 / 4297

页数：17

共 63 条

[1]

[Anonymous], 1982, EOS T AM GEOPHYS UN

[2]

Bell T. H, 1973, LITHOS, V6, P337, DOI DOI 10.1016/0024-4937(73)90052-2

[3] PLASTICITY AND HYDROLYTIC WEAKENING OF QUARTZ SINGLE-CRYSTALS [J].

BLACIC, JD ;

CHRISTIE, JM .

JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB6) :4223-4239

[4] SP-MYLONITES - ORIGIN OF SOME MYLONITES BY SUPERPLASTIC FLOW [J].

BOULLIER, AM ;

GUEGUEN, Y .

CARISTAN, Y .

JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB8) :6781-6790

[6]

CASE ED, 1981, AM CERAM SOC COMMUN, V64, pC24

[7]

Chadwick G. A., 1976, GRAIN BOUNDARY STRUC

[8]

CHRISTIE JM, 1980, EOS, V61, P377

[9]

CHRISTIE JM, 1979, EOS T AGU, V60, P948

[10]

CLARKE FW, 1924, US GEOL SURV B, V770