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
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VIDAL M, 1986, J AFR EARTH SCI, V6, P141
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ZONOU S, 1987, THESIS U NANCY 1