《Table 1 The dihedral angles vs.faults at the top of the Ordovician carbonate in Halahatang area》

《Table 1 The dihedral angles vs.faults at the top of the Ordovician carbonate in Halahatang area》   提示：宽带有限、当前游客访问压缩模式
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《"The Dihedral Angle and Intersection Processes of a Conjugate Strike-Slip Fault System in the Tarim Basin, NW China"》


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The dihedral angles of the conjugate faults show a strong negative correlation with the strike of NW-SE trending faults，but a weak positive correlation with the strike of NE-SW trending faults（Figs.7a，7b；Table1）.This suggests the dihedral angles are related to the orientation of the NW trending faults more than to the NE trending faults.Taken together，except for a few scattered data mostly attributable to small irregular faults，conjugate fault dihedral angles demonstrate a good correlation with the orientation of major faults.This suggests major fault orientation is a controlling factor on dihedral angles.

图表编号XD0017166600    严禁用于非法目的
绘制时间2018.02.01
作者WU Guanghui、YUAN Yajuan、HUANG Shaoying、Thomas Matthew VANDyk、XIAO Yang、CAI Quan、LUO Bingxu
绘制单位Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, School of Marine Sciences, Sun Yat-sen University、Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, School of Marine Sciences, Sun Yat-sen Univ
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