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- W2371952031 abstract "Eastern Hunan－western Jiangxi(EHWJ) is an important site of Tan－Lu fault south elongation.Since Mesozoic Era the NNE－trending left－lateral strike－slip tectonics (NNE－SST) are mainly compounded of T3～ J convergent SST and K～ E divergent SST. The convergent strike－slip faulting resulted in a large amount of en echelon folds and faults, remelted granites, shear curve and rotation structures as well as compressive－shear coal basins. The divergent strike－slip faulting directly controlled formation and distribution of significant polymetallic hydrothermal deposits,“ basin－range type tectonic landforms and shear－tensional red basins.The reason of more complicated wrench tectonics in EHWJ than that in Tan－Lu area was mainly related to the differences of the crust structural layer,pre－existing fault style, displacement and strike－slip tectonic formation history between these two areas." @default.
- W2371952031 created "2016-06-24" @default.
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- W2371952031 date "2001-01-01" @default.
- W2371952031 modified "2023-09-23" @default.
- W2371952031 title "STRIKE－SLIP TECTONICS TRENDING NNE IN THE AREA OF EASTERN HUNAN AND WESTERN JIANGXI,CHINA" @default.
- W2371952031 hasPublicationYear "2001" @default.
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