TRANSCURRENT EBURNEAN TECTONICS IN WEST AFRICA - EXAMPLE OF THE DJIBO AREA (BURKINA-FASO)

被引：0
作者：
NIKIEMA, S
BENKHELIL, J
CORSINI, M
BOURGES, F
DIA, A
MAURIN, JC
机构：
[1] UNIV OUAGADOUGOU,DEPT GEOL,OUAGADOUGOU,BURKINA FASO
[2] UNIV CHEIKH ANTA DIOP,DEPT GEOL,DAKAR,SENEGAMBIA
[3] UNIV PERPIGNAN,SEDIMENTOL & GEOCHIM MARINES LAB,F-66025 PERPIGNAN,FRANCE
来源：
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1993年 / 316卷 / 05期
关键词：
D O I：
暂无
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
The transcurrent tectonics in the Djibo area is characterized by sub-meridian sinistral ductile shear zones. The characteristics of the deformation affecting the shear zones in low-grade metamorphic conditions are defined This major tectonic event is known in throughout West Africa and corresponds to the Eburnean orogeny.
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页码：661 / 668
页数：8
相关论文
共 22 条
  • [1] ABOUCHAMI W, 1992, 14E REUN SCI TERR TO, P1
  • [2] BERTRAND JM, 1989, CR ACAD SCI II, V309, P751
  • [3] BOHER M, 1991, THESIS U NANCY 1 FRA
  • [4] PLASTIC-DEFORMATION OF QUARTZITES AT LOW-TEMPERATURE IN AN AREA OF NATURAL STRAIN GRADIENT
    BOUCHEZ, JL
    [J]. TECTONOPHYSICS, 1977, 39 (1-3) : 25 - 50
  • [5] DUCELLIER J, 1963, MEM BRGM, V10
  • [6] FABRE R, 1985, CR ACAD SCI II, V300, P955
  • [7] FABRE R, 1990, CR ACAD SCI II, V311, P971
  • [8] FEYBESSE JL, 1990, CR ACAD SCI II, V310, P1353
  • [9] FEYBESSE JL, 1989, CR ACAD SCI II, V309, P1847
  • [10] TRANSCURRENT TECTONICS AND POLYCYCLIC EVOLUTION IN THE LOWER PROTEROZOIC OF SENEGAL-MALI
    LEDRU, P
    PONS, J
    MILESI, JP
    FEYBESSE, JL
    JOHAN, V
    [J]. PRECAMBRIAN RESEARCH, 1991, 50 (3-4) : 337 - 354
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