LACK OF PORPHYROBLAST ROTATION IN THE OTAGO SCHISTS, NEW-ZEALAND - IMPLICATIONS FOR CRENULATION CLEAVAGE DEVELOPMENT, FOLDING AND DEFORMATION PARTITIONING

被引:61
作者
JOHNSON, SE
机构
[1] Department of Geology, James Cook University, Townsville, Queensland
关键词
continuum mechanics; crenulation cleavage; deformation partitioning; garnet; Key‐words: albite; lack of porphyroblast rotation; Otago schists; sense of shear; sequential growth;
D O I
10.1111/j.1525-1314.1990.tb00454.x
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Porphyroblasts of garnet and plagioclase in the Otago schists have not rotated relative to geographic coordinates during non‐coaxial deformation that post‐dates their growth. Inclusion trails in most of the porphyroblasts are oriented near‐vertical and near‐horizontal, and the strike of near‐vertical inclusion trails is consistent over 3000 km2. Microstructural relationships indicate that the porphyroblasts grew in zones of progressive shortening strain, and that the sense of shear affecting the geometry of porphyroblast inclusion trails on the long limbs of folds is the same as the bulk sense of displacement of fold closures. This is contrary to the sense of shear inferred when porphyroblasts are interpreted as having rotated during folding. Several crenulation cleavage/fold models have previously been developed to accommodate the apparent sense of rotation of porphyroblasts that grew during folding. In the light of accumulating evidence that porphyroblasts do not generally rotate, the applicability of these models to deformed rocks is questionable. Whether or not porphyroblasts rotate depends on how deformation is partitioned. Lack of rotation requires that progressive shearing strain (rotational deformation) be partitioned around rigid heterogeneities, such as porphyroblasts, which occupy zones of progressive shortening or no strain (non‐rotational deformation). Therefore, processes operating at the porphyroblast/matrix boundary are important considerations. Five qualitative models are presented that accommodate stress and strain energy at the boundary without rotating the porphyroblast: (a) a thin layer of fluid at the porphyroblast boundary; (2) grain‐boundary sliding; (3) a locked porphyroblast/matrix boundary; (4) dissolution at the porphyroblast/matrix boundary, and (5) an ellipsoidal porphyroblast/shadow unit. Copyright © 1990, Wiley Blackwell. All rights reserved
引用
收藏
页码:13 / 30
页数:18
相关论文
共 71 条
[1]   SLENDER-BODY THEORY FOR PARTICLES OF ARBITRARY CROSS-SECTION IN STOKES FLOW [J].
BATCHELOR, GK .
JOURNAL OF FLUID MECHANICS, 1970, 44 (NOV26) :419-+
[2]   DISSOLUTION, SOLUTION TRANSFER, DIFFUSION VERSUS FLUID-FLOW AND VOLUME LOSS DURING DEFORMATION METAMORPHISM [J].
BELL, TH ;
CUFF, C .
JOURNAL OF METAMORPHIC GEOLOGY, 1989, 7 (04) :425-447
[3]   PORPHYROBLAST INCLUSION TRAILS - THE KEY TO OROGENESIS [J].
BELL, TH ;
JOHNSON, SE .
JOURNAL OF METAMORPHIC GEOLOGY, 1989, 7 (03) :279-310
[4]   PORPHYROBLAST NUCLEATION, GROWTH AND DISSOLUTION IN REGIONAL METAMORPHIC ROCKS AS A FUNCTION OF DEFORMATION PARTITIONING DURING FOLIATION DEVELOPMENT [J].
BELL, TH ;
RUBENACH, MJ ;
FLEMING, PD .
JOURNAL OF METAMORPHIC GEOLOGY, 1986, 4 (01) :37-67
[5]   SEQUENTIAL PORPHYROBLAST GROWTH AND CRENULATION CLEAVAGE DEVELOPMENT DURING PROGRESSIVE DEFORMATION [J].
BELL, TH ;
RUBENACH, MJ .
TECTONOPHYSICS, 1983, 92 (1-3) :171-194
[7]   DEFORMATION PARTITIONING AND PORPHYROBLAST ROTATION IN METAMORPHIC ROCKS - A RADICAL REINTERPRETATION [J].
BELL, TH .
JOURNAL OF METAMORPHIC GEOLOGY, 1985, 3 (02) :109-118
[8]   FOLIATION DEVELOPMENT AND REFRACTION IN METAMORPHIC ROCKS - REACTIVATION OF EARLIER FOLIATIONS AND DECRENULATION DUE TO SHIFTING PATTERNS OF DEFORMATION PARTITIONING [J].
BELL, TH .
JOURNAL OF METAMORPHIC GEOLOGY, 1986, 4 (04) :421-444
[9]   DEFORMATION PARTITIONING, SHEAR ZONE DEVELOPMENT AND THE ROLE OF UNDEFORMABLE OBJECTS [J].
BELL, TH ;
DUNCAN, AC ;
SIMMONS, JV .
TECTONOPHYSICS, 1989, 158 (1-4) :163-171
[10]   STRAIN-INDUCED PREFERENTIAL DISSOLUTION OF HALITE [J].
BOSWORTH, W .
TECTONOPHYSICS, 1981, 78 (1-4) :509-525