Grain reduction and growth in faulting and new classification of faulted rocks

Jiarui Duan , Hua Kong

Journal of Central South University ›› 1996, Vol. 3 ›› Issue (1) : 44 -46.

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Journal of Central South University ›› 1996, Vol. 3 ›› Issue (1) : 44 -46. DOI: 10.1007/BF02652056
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Grain reduction and growth in faulting and new classification of faulted rocks

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Abstract

New classification scheme about faulted rocks is proposed, according to the extent of grain reduction and growth and their sequence, and faulted rocks are classified as follows: (1) faulted rocks formed by the reduction action mainly include breccia series, cataclasite series, tectonobutchite series, mylonite series; (2) faulted rocks formed by growth action is mainly tectono-schist (gneiss) series; (3) blastomylonite series formed by grain reduction first and then growth; (4) mylonitic schist (gneiss) series formed by crystal growth first and then grain reduction. All series can be further classified according to matrix contents.

Keywords

reduction / growth / faulting / classification

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Jiarui Duan, Hua Kong. Grain reduction and growth in faulting and new classification of faulted rocks. Journal of Central South University, 1996, 3(1): 44-46 DOI:10.1007/BF02652056

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References

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SibsonR H. Fault rocks and fault mechanism. J Geol Soc London, 1977, 133: 191-213

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WiseD V, DunnD E, EngelderJ T, et al.. Fault-related, suggestion for terminology. Geology, 1984, 12: 391-394

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SongHonglin. Commentary about the classification of faulted rocks. Geological Science and Technology Information, 1986, 5(1): 21-26(in Chinese)

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GuoBaoluo, ZhongZengqui, LiZhizhong. Primary discussion about the classification of faulted structural rocks. Earth Science, 1987, 4(1): 31-38(in Chinese)

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