THE MAXIMUM-EFFECTIVE-MOMENT CRITERION DEVELOPING IN PRACTICE

ZHENG Ya-dong; ZHANG Jin-jiang; WANG Tao

Volume 15 Issue 3

Sep. 2009

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ZHENG Ya-dong, ZHANG Jin-jiang, WANG Tao, 2009. THE MAXIMUM-EFFECTIVE-MOMENT CRITERION DEVELOPING IN PRACTICE. Journal of Geomechanics, 15 (3): 209-217.

Citation:

ZHENG Ya-dong, ZHANG Jin-jiang, WANG Tao, 2009. THE MAXIMUM-EFFECTIVE-MOMENT CRITERION DEVELOPING IN PRACTICE. Journal of Geomechanics, 15 (3): 209-217.

Citation:

ZHENG Ya-dong, ZHANG Jin-jiang, WANG Tao, 2009. THE MAXIMUM-EFFECTIVE-MOMENT CRITERION DEVELOPING IN PRACTICE. Journal of Geomechanics, 15 (3): 209-217.

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THE MAXIMUM-EFFECTIVE-MOMENT CRITERION DEVELOPING IN PRACTICE

1.
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

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Received: 2009-05-19
Published: 2009-09-01

Abstract

Abstract

Since the Maximum-Effective-Moment Criterion was published, it has been obtaining evidence in nature and the laboratory and supports from geologists home and abroad. Behavior of rock during deformation depends on mechanical property itself, structure levels (including such factors as temperature, pressure, fluid) and strain rate. The lozenge features and conjugate kink zones with obtuse angles in the contractional direction at shallow levels are consistent with the criterion and suggested as deformation at low strain rates and conform that the strain rate plays a more important role than the structure level in deformation. Coexistence of brittle and ductile features implies a tectonic evolution with alternation of high and low strain rates.
- Maximum-Effective-Moment Criterion,
- strain rates,
- kink belt,
- lozenge features

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References(30)

References

[1]	Zheng Y, Wang T, Ma M, et al.Maximum effective moment criterion and the origin of low-angle normal faults[J].J.Struct. Geol., 2004, 26:271 (285. doi: 10.1016/S0191-8141(03)00079-8
[2]	《地球科学大辞典》编委会.地球科学大词典[M].北京:地质出版社, 2005. 1~823. Editorial Committee of 《Dictionary of Earth Sciences》.Dictionary of Earth Sciences[M].Beijing:Geological Publishing House, 2005.1~823.
[3]	Twiss R J, Moores E M, Structural Geology (Second Edition)[M].New York:W H Freeman and Company, 2005.
[4]	曾佐勋, 樊光明.构造地质学(第三版)[M].武汉:中国地质大学出版社, 2006. ZENG Zuo-xun, FAN Guang-ming.Structural Geology (Third Edition)[M].Wuhan:China University of Geosciences Press, 2006.
[5]	中国地质学会构造地质学与地球动力学专业委员会. 构造地质学的成就与前景[A]. 见: 中国科学技术协会, 中国地质学会编. 2006~2007地质学学科发展报告[C]. 北京: 中国科学技术出版社, 2007. 67~78. Structural Geology and Geodynamics Professional Committee of Geological Society of China. Achievement and prospects on structural geology[A]. In: China Association for Science and Technology, Geological Society of China. 2006~2007 Report on Advances in Geological Sciences[C]. Beijing: China Science and Technology Press, 2007. 67~78.
[6]	Neves S P, da Silva J M R, Mariano G.Oblique lineations in orthogneisses and supracrustal rocks:vertical partitioning of strain in a hot crust (eastern Borboroma Province, NE Brazil)[J].J.Structural Geology, 2005, 27 (8):1513~1527. doi: 10.1016/j.jsg.2005.02.002
[7]	Guo Z J, Shi H Y, Zhang Z C, et al.The tectonic evolution of the north Tianshan paleo-oceanic crust inferred from spreading structures and Ar-Ar dating of the Hongliuge ophiolite, NW China[J].Acta Petrologica Sinica, 2006, 22 (1):75~102. http://www.oalib.com/paper/1472073
[8]	Marshak S, Alkmin F F, Whittington A, et al.Extensional collapse in the Neoproterozoic Aracual orogen, eastern Brazil:a setting for reactivation of a symmetric crenulation cleavage[J].Journal of Structural Geology, 2006, 28 (1):129~147. doi: 10.1016/j.jsg.2005.09.006
[9]	Yang T N, Wang Y, Li J Y, et al.Vertical and horizontal strain partitioning of the central Tianshan (NW China):Evidence fr om structures and Ar40-Ar39 geochronology[J].Journal of Structural Geology, 2007, 29 (10):1605~1621. doi: 10.1016/j.jsg.2007.08.002
[10]	King D S, Klepeis K A, Goldstien AG, et al.The initiation and evolution of the transpressional Straight River shear zone, Central Fjordland, New Zealand[J].Journal of Structural Geology, 2008, 30 (4):410~430. doi: 10.1016/j.jsg.2007.12.004
[11]	Fowler A, Osman A F.The Sha'it-Nugrus Shear zone separating Central and South Eastern Deserts, Egypt:A post-arc collision low-angle normal ductile shear zone[J].Journal of African Earth S ciences, 2009, 52 (1~2):16~32. http://www.sciencedirect.com/science/article/pii/S1464343X08001076
[12]	Kurz G.A, Northrup C J.Structural analysis of mylonitic rocks in the Cougar Creek Complex, Oregon-Idaho using the porphyroclast hyperbolic distribution method, and potential use of SC' -type extensional shear bands as quantitative vorticity indicators[J].Journal of Structural Geology, 2008.30 (8):1005~1012. doi: 10.1016/j.jsg.2008.04.003
[13]	Vernooij M G C, Kunze K, den Brok B.Brittle'shear zones in experimentally deformed quartz single crystals[J].Journal of Structural Geology, 2006, 28 (7):1292~1306. doi: 10.1016/j.jsg.2006.03.018
[14]	Watterson J.The future of failure:stress or strain?[J] Journal of Structural Geology, 1999, 21:139 (148. doi: 10.1016/S0191-8141(98)00111-4
[15]	Park RG.Shear-zone deformation and bulk strain in granite-greenstone terrain of the Western Superior Province[J].Canada. Pr ecambrian Research, 1981, 14:31~47. http://www.sciencedirect.com/science/article/pii/0301926881900346
[16]	Sibson R H.Fault rocks and fault mechanisms[J].Journal of the Geological Society, 1977, 133 (3):191~213. doi: 10.1144/gsjgs.133.3.0191
[17]	Ujiie K, Malman A J, Sanchez-Gomez M.Origin of deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism, southwest Japan[J].J.Struct.Geol., 2004, 26:221~231. doi: 10.1016/j.jsg.2003.06.001
[18]	Camerlo R H, Benson E F.Geometric and seismic interpretation of Perdido fold belt:Northwestern deep-water Gulf of Mexico [J].AAPG Bulletin, 2006, 90 (3):363~386. doi: 10.1306/10120505003
[19]	郑亚东, 王涛, 王新社.最大有效力矩准则的理论与实践[J].北京大学学报(自然科学版), 2007, 43 (2): 145~156. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=bjdz200702000&dbname=CJFD&dbcode=CJFQ ZHENG Ya-dong, WANG Tao, WANG Xin-she.Theory and Practice of the Maximum Effective Moment Criterion(MEMC)[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 2007, 43 (2):145~156. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=bjdz200702000&dbname=CJFD&dbcode=CJFQ
[20]	郑亚东, 莫午零, 张文涛, 等.柴达木盆地油气勘探的新思路[J].石油勘探与开发, 2007, 34 (1):13~18. http://en.cnki.com.cn/Article_en/CJFDTotal-SKYK200701003.htm ZHENG Ya-dong, MO Wu-ling, ZHENG Wen-tao, et al.A new idea for petroleum exploration in Qaidam Basin[J]. Petroleum Exploration and Development, 2007, 34 (1):13~18. http://en.cnki.com.cn/Article_en/CJFDTotal-SKYK200701003.htm
[21]	Paterson M S, Weiss LE.Experimental deformation and folding in phyllite[J].Geological Society of America Bulletin, 1966, 77:343 (374. doi: 10.1130/0016-7606(1966)77[343:EDAFIP]2.0.CO;2
[22]	Ramsay J G, Huber M I.The Techniques of Modern Structural Geology Fractures.Volume 2:Folds and Fractures[M].New York:Academic Press, 1987.
[23]	Tapponnier P, Molnar P.Slip-line field theory and large-scale continental tectonics[J].Nature, 1976, 264:319~324. doi: 10.1038/264319a0
[24]	Hill R.The Mathematical Theory of Plasticity[M].Oxford:Oxford University Press/Clarendon Press, 1950.
[25]	Tapponnier P, Peltzer G., Le Dain A Y, et al., Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine[J].Geology, 1982, 10:611~616. doi: 10.1130/0091-7613(1982)10<611:PETIAN>2.0.CO;2
[26]	Kapp P, Taylor M, Stockli D, et al.Development of active low-angle normal fault systems during orogenic collapse:insight from Tibet[J].Geology, 2008, 36:7~10. doi: 10.1130/G24054A.1
[27]	Wright T J, Parsons B, England P C, et al.InSAR observations of low slip rates on the major faults of west Tibet[J].Science, 2004, 305:236~239. doi: 10.1126/science.1096388
[28]	McKenzie D P.Plate tectonics of the Mediterranean region[J].Nature, 1970, 226:239~243. doi: 10.1038/226239a0
[29]	McKenzie D P.Active tectonics of the Mediterranean region[J].Geophysical Journal International, 1972, 30 (2):109~185. doi: 10.1111/j.1365-246X.1972.tb02351.x
[30]	McClusky S, Balassanian S, Barka A, et al.Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and Caucasus[J].Journal of Geophysical Research, 2000, 105 (B3), 5695~5720. doi: 10.1029/1999JB900351