DING Yuan-chen, WANG Xi-hai, HE Pei-yuan, 2001. THE SWAYING PROBLEM OF UNIVERSAL TESTING MACHINE IN THE MEASUREMENT OF ROCK STRESS BY AE METHOD DING Yuan-chen,WANG Xi-hai,HE Pei-yuan. Journal of Geomechanics, 7 (4): 346-350.
Citation: CUI Runze, WEI Chunjing, 2023. Evolution of metamorphic processes in the Neoarchean mafic granulites of the Qingyuan Terrane in northern Liaoning, North China Craton. Journal of Geomechanics, 29 (5): 736-756. DOI: 10.12090/j.issn.1006-6616.2023049

Evolution of metamorphic processes in the Neoarchean mafic granulites of the Qingyuan Terrane in northern Liaoning, North China Craton

doi: 10.12090/j.issn.1006-6616.2023049
Funds:

the Funds of the National Natural Science Foundation of China 41872057

the Funds of the National Natural Science Foundation of China 418930834

More Information
  • Multiple interpretations exist regarding the tectonic evolution model of the Neoarchean North China Craton, requiring a more in-depth study of metamorphic processes. Systematic petrographic observations, mineral chemical analysis, phase equilibrium modeling, and zircon dating were conducted on the basic granulites from Qingyuan in northern Liaoning to elucidate their metamorphic evolution processes and geological significance. The selected samples of mafic granulites were divided into the garnet-bearing domain (19DJ07-GD) and garnet-free domain (19DJ07-NGD), with the garnet-bearing region displaying a banded and inhomogeneous distribution. Both domains exhibit two generations of granulite facies assemblages. In the garnet-bearing domain, the first-generation metamorphic mineral assemblage includes garnet + clinopyroxene + orthopyroxene + hornblende + biotite + plagioclase + quartz. Notably, the first-generation plagioclase (Pl1) exhibits a complex compositional zoning, with anorthite content (xAn) increasing from the core to the mantle and then decreasing towards the rim. Similarly, the titanium component zoning in the first-generation amphibole (Amp1) follows a pattern of increasing from the core to the mantle and then decreasing towards the rim. Based on mineral assemblages and corresponding component zoning, it is inferred that the first-generation granulite facies metamorphic process followed a counterclockwise P-Tpath, involving a pre-peak P-T rise stage and a post-peak P-T drop stage. Phase equilibrium modeling constrains the peak conditions at 0.8~0.9 GPa/900~950 ℃, indicative of high-ultrahigh-temperature (HT-UHT) metamorphism conditions. Zircon dating results yielded a post-peak cooling age of 2498±6.9 Ma (MSWD=0.39). Considering the regional "dome-and-keel" tectonics, the counterclockwise P-T path, and the metamorphic timing of supracrustal rock nearly synchronous with late-stage TTG magmatic pulses, the UHT metamorphism of the supracrustal rocks is believed to be controlled by the unique Archean vertical tectonics/sagduction system. The second-generation metamorphic assemblage is characterized by locally formed coronas or symplectites of garnet + quartz ± clinopyroxene, representing high-pressure (HP) granulite facies metamorphism associated with a Paleoproterozoic orogenic event.

     

  • Full-text Translaiton by iFLYTEK

    The full translation of the current issue may be delayed. If you encounter a 404 page, please try again later.
  • ANHAEUSSER C R, 2014. Archaean greenstone belts and associated granitic rocks-a review[J]. Journal of African Earth Sciences, 100: 684-732. doi: 10.1016/j.jafrearsci.2014.07.019
    BAI X, LIU S W, YAN M, et al., 2014. Geological event series of Early Precambrian metamorphic complex in South Fushun area, Liaoning province[J]. Acta Petrologica Sinica, 30(10): 2905-2924. (in Chinese with English abstract)
    BROWN M, 2007. Metamorphic conditions in orogenic belts: a record of secular change[J]. International Geology Review, 49(3): 193-234. doi: 10.2747/0020-6814.49.3.193
    BROWN M, JOHNSON T, 2018. Secular change in metamorphism and the onset of global plate tectonics[J]. American Mineralogist, 103(2): 181-196. doi: 10.2138/am-2018-6166
    CAO Y, SONG S G, NIU Y L, et al., 2011. Variation of mineral composition, fabric and oxygen fugacity from massive to foliated eclogites during exhumation of subducted ocean crust in the North Qilian suture zone, NW China[J]. Journal of Metamorphic Geology, 29(7): 699-720. doi: 10.1111/j.1525-1314.2011.00937.x
    COLLINS W J, VAN KRANENDONK M J, TEYSSIER C, 1998. Partial convective overturn of Archaean crust in the east Pilbara Craton, Western Australia: driving mechanisms and tectonic implications[J]. Journal of Structural Geology, 20(9-10): 1405-1424. doi: 10.1016/S0191-8141(98)00073-X
    CONDIE K C, 1981. Archean greenstone belts[M]. Amsterdam: Elsevier.
    CORFU F, HANCHAR J M, HOSKIN P W O, et al., 2003. Atlas of zircon textures[J]. Reviews in Mineralogy and Geochemistry, 53(1): 469-500. doi: 10.2113/0530469
    DOS SANTOS T M B, MUNHÁ J M U, TASSINARI C C G, et al., 2011. P-T-fluid evolution and graphite deposition during retrograde metamorphism in Ribeira fold belt, SE Brazil: oxygen fugacity, fluid inclusions and C-O-H isotopic evidence[J]. Journal of South American Earth Sciences, 31(1): 93-109. doi: 10.1016/j.jsames.2010.02.002
    DUAN Z Z, WEI C J, REHMAN H U, 2017. Metamorphic evolution and zircon ages of pelitic granulites in eastern Hebei, North China Craton: insights into the regional Archean P-T-t history[J]. Precambrian Research, 292: 240-257. doi: 10.1016/j.precamres.2017.02.008
    DUAN Z Z, WEI C J, LI Z, 2019. Metamorphic P-T paths and zircon u-pb ages of Paleoproterozoic metabasic dykes in eastern Hebei and northern Liaoning: Implications for the tectonic evolution of the North China Craton[J]. Precambrian Research, 326: 124-141. doi: 10.1016/j.precamres.2017.11.001
    FRANÇOIS C, PHILIPPOT P, REY P, et al., 2014. Burial and exhumation during Archean sagduction in the East Pilbara granite-greenstone terrane[J]. Earth and Planetary Science Letters, 396: 235-251. doi: 10.1016/j.epsl.2014.04.025
    GENG Y S, LIU F L, YANG C H, 2006. Magmatic event at the end of the Archean in eastern Hebei Province and its geological implication[J]. Acta Geologica Sinica, 80(6): 819-833. doi: 10.1111/j.1755-6724.2006.tb00305.x
    GREEN E C R, WHITE R W, DIENER J F A, et al., 2016. Activity-composition relations for the calculation of partial melting equilibria in metabasic rocks[J]. Journal of Metamorphic Geology, 34(9): 845-869. doi: 10.1111/jmg.12211
    HAWTHORNE F C, OBERTI R, HARLOW G E, et al., 2012. Nomenclature of the amphibole supergroup[J]. American Mineralogist, 97(11-12): 2031-2048. doi: 10.2138/am.2012.4276
    HICKMAN A H, 2004. Two contrasting granite- greenstone terranes in the Pilbara Craton, Australia: evidence for vertical and horizontal tectonic regimes prior to 2900 Ma[J]. Precambrian Research, 131(3-4): 153-172. doi: 10.1016/j.precamres.2003.12.009
    HOLLAND T, POWELL R, 2003. Activity-composition relations for phases in petrological calculations: an asymmetric multicomponent formulation[J]. Contributions to Mineralogy and Petrology, 145(4): 492-501. doi: 10.1007/s00410-003-0464-z
    HOLLAND T J B, POWELL R, 1998. An internally consistent thermodynamic data set for phases of petrological interest[J]. Journal of Metamorphic Geology, 16(3): 309-343. doi: 10.1111/j.1525-1314.1998.00140.x
    HOLLAND T J B, POWELL R, 2011. An improved and extended internally consistent thermodynamic dataset for phases of petrological interest, involving a new equation of state for solids[J]. Journal of Metamorphic Geology, 29(3): 333-383. doi: 10.1111/j.1525-1314.2010.00923.x
    JAYANANDA M, BANERJEE M, PANT NC, et al., 2012. 2.62 Ga high-temperature metamorphism in the central part of the Eastern Dharwar Craton: implications for late Archaean tectonothermal history[J]. Geological Journal, 47(2-3): 213-236. doi: 10.1002/gj.1308
    KELSEY D E, POWELL R, 2011. Progress in linking accessory mineral growth and breakdown to major mineral evolution in metamorphic rocks: A thermodynamic approach in the Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-ZrO2 system[J]. Journal of Metamorphic Geology, 29(1): 151-166. doi: 10.1111/j.1525-1314.2010.00910.x
    KORHONEN F J, POWELL R, STOUT J H, 2012. Stability of sapphirine + quartz in the oxidized rocks of the Wilson Lake terrane, Labrador: calculated equilibria in NCKFMASHTO[J]. Journal of Metamorphic Geology, 30(1): 21-36. doi: 10.1111/j.1525-1314.2011.00954.x
    KORHONEN F J, BROWN M, CLARK C, et al., 2013. Osumilite-melt interactions in ultrahigh temperature granulites: Phase equilibria modelling and implications for the P-T-t evolution of the Eastern Ghats Province, India[J]. Journal of Metamorphic Geology, 31(8): 881-907. doi: 10.1111/jmg.12049
    KUSKY T M, LI J H, 2003. Paleoproterozoic tectonic evolution of the North China Craton[J]. Journal of Asian Earth Sciences, 22(4): 383-397. doi: 10.1016/S1367-9120(03)00071-3
    KUSKY T M, POLAT A, WINDLEY B F, et al., 2016. Insights into the tectonic evolution of the North China Craton through comparative tectonic analysis: a record of outward growth of Precambrian continents[J]. Earth-Science Reviews, 162: 387-432. doi: 10.1016/j.earscirev.2016.09.002
    KWAN L C J, ZHAO G C, YIN C Q, et al., 2016. Metamorphic P-T path of mafic granulites from Eastern Hebei: implications for the Neoarchean tectonics of the Eastern Block, North China Craton[J]. Gondwana Research, 37: 20-38. doi: 10.1016/j.gr.2016.05.004
    LAMBERT I B, WYLLIE P J, 1972. Melting of gabbro (quartz eclogite) with excess water to 35 kilobars, with geological applications[J]. The Journal of Geology, 80(6): 693-708. doi: 10.1086/627795
    LI Z, WEI C J, 2017. Two types of Neoarchean basalts from Qingyuan greenstone belt, North China Craton: petrogenesis and tectonic implications[J]. Precambrian Research, 292: 175-193. doi: 10.1016/j.precamres.2017.01.014
    LI Z, WEI C J, CHEN B, et al., 2020. Late Neoarchean reworking of the Mesoarchean crustal remnant in northern Liaoning, North China Craton: a U-Pb-Hf-O-Nd perspective[J]. Gondwana Research, 80: 350-369. doi: 10.1016/j.gr.2019.10.020
    LIN S F, BEAKHOUSE G P, 2013. Synchronous vertical and horizontal tectonism at late stages of Archean cratonization and genesis of Hemlo gold deposit, Superior craton, Ontario, Canada[J]. Geology, 41(3): 359-362. doi: 10.1130/G33887.1
    LIU J, BOHLEN S R, ERNST W G, 1996. Stability of hydrous phases in subducting oceanic crust[J]. Earth and Planetary Science Letters, 143(1-4): 161-171. doi: 10.1016/0012-821X(96)00130-6
    LIU T, WEI C J, 2018. Metamorphic evolution of Archean ultrahigh-temperature mafic granulites from the western margin of Qian'an gneiss dome, eastern Hebei Province, North China Craton: insights into the Archean tectonic regime[J]. Precambrian Research, 318: 170-187. doi: 10.1016/j.precamres.2018.10.007
    LIU T, WEI C J, 2020. Metamorphic P-T paths and Zircon U-Pb ages of Archean ultra-high temperature paragneisses from the Qian'an gneiss dome, East Hebei terrane, North China Craton[J]. Journal of Metamorphic Geology, 38(4): 329-356. doi: 10.1111/jmg.12524
    LIU T, WEI C J, KRÖNER A, et al., 2020. Metamorphic P-T paths for the Archean Caozhuang supracrustal sequence, eastern Hebei Province, North China Craton: implications for a sagduction regime[J]. Precambrian Research, 340: 105346. doi: 10.1016/j.precamres.2019.105346
    LIU T, WEI C J, JOHNSON T E, et al., 2022a. Newly-discovered ultra-high temperature granulites from the East Hebei terrane, North China Craton[J]. Science Bulletin, 67(7): 670-673. doi: 10.1016/j.scib.2021.12.023
    LIU T, LI Z, WEI C J, 2022b. Metamorphic evolution of the archean supracrustal rocks from the Qingyuan Area of the Northern Liaoning Terrane, North China Craton: constrained using phase equilibrium modeling and monazite dating[J]. Minerals, 12(9): 1079. doi: 10.3390/min12091079
    LU H S, WEI C J, 2020. Late Neoarchean or late Paleoproterozoic high-pressure granulite facies metamorphism from the East Hebei terrane, North China Craton? [J]. Journal of Asian Earth Sciences, 190: 104195. doi: 10.1016/j.jseaes.2019.104195
    MEZGER K, BOHLEN S R, HANSON G N, 1990. Metamorphic history of the Archean Pikwitonei granulite domain and the Cross Lake Subprovince, Superior Province, Manitoba, Canada[J]. Journal of Petrology, 31(2): 483-517. doi: 10.1093/petrology/31.2.483
    MORIMOTO N, 1988. Nomenclature of pyroxenes[J]. Mineralogy and Petrology, 39(1): 55-76. doi: 10.1007/BF01226262
    NEMCHIN A A, GIANNINI L M, BODORKOS S, et al., 2001. Ostwald ripening as a possible mechanism for zircon overgrowth formation during anatexis: theoretical constraints, a numerical model, and its application to pelitic migmatites of the Tickalara Metamorphics, northwestern Australia[J]. Geochimica et Cosmochimica Acta, 65(16): 2771-2788. doi: 10.1016/S0016-7037(01)00622-6
    PENG P, WANG C, WANG X P, et al., 2015. Qingyuan high-grade granite-greenstone terrain in the eastern North China Craton: root of a Neoarchaean arc[J]. Tectonophysics, 662: 7-21. doi: 10.1016/j.tecto.2015.04.013
    ROBERTS M P, FINGER F, 1997. Do U-Pb zircon ages from granulites reflect peak metamorphic conditions? [J]. Geology, 25(4): 319-322. doi: 10.1130/0091-7613(1997)025<0319:DUPZAF>2.3.CO;2
    RUBATTO D, 2002. Zircon trace element geochemistry: partitioning with garnet and the link between U-Pb ages and metamorphism[J]. Chemical Geology, 184(1-2): 123-138. doi: 10.1016/S0009-2541(01)00355-2
    SAJEEV K, OSANAI Y, KON Y, et al., 2009. Stability of pargasite during ultrahigh-temperature metamorphism: A consequence of titanium and REE partitioning? [J]. American Mineralogist, 94(4): 535-545. doi: 10.2138/am.2009.2815
    SEN C, DUNN T, 1994. Dehydration melting of a basaltic composition amphibolite at 1.5 and 2.0 GPa: implications for the origin of adakites[J]. Contributions to Mineralogy and Petrology, 117(4): 394-409. doi: 10.1007/BF00307273
    SLÁMA J, KOŠLER J, CONDON D J, et al., 2008. Plešovice zircon—a new natural reference material for U-Pb and Hf isotopic microanalysis[J]. Chemical Geology, 249(1-2): 1-35. doi: 10.1016/j.chemgeo.2007.11.005
    SUN S S, MCDONOUGH W F, 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[J]. Geological Society, London, Special Publications, 42(1): 313-345. doi: 10.1144/GSL.SP.1989.042.01.19
    VAVRA G, SCHMID R, GEBAUER D, 1999. Internal morphology, habit and U-Th-Pb microanalysis of amphibolite-to-granulite facies zircons: geochronology of the Ivrea Zone (Southern Alps)[J]. Contributions to Mineralogy and Petrology, 134(4): 380-404. doi: 10.1007/s004100050492
    WAN Y S, SONG B, GENG Y S, et al., 2005a. Geochemical characteristics of Archaean basement in the Fushun-Qingyuan area, Northern Liaoning Province and its geological significance[J]. Geological Review, 51(2): 128-137. (in Chinese with English abstract)
    WAN Y S, SONG B, YANG C, et al., 2005b. Zircon SHRIMP U-Pb geochronology of Archaean rocks from the Fushun-Qingyuan area, Liaoning Province and its geological significance[J]. Acta Geologica Sinica, 79(1): 78-87. (in Chinese with English abstract)
    WAN Y S, DONG C Y, XIE H Q, et al., 2022. Huge growth of the late Mesoarchean-early Neoarchean (2.6~3.0 Ga) continental crust in the North China Craton: a review[J]. Journal of Geomechanics, 28(5): 866-906, doi: 10.12090/j.issn.1006-6616.20222817. (in Chinese with English abstract)
    WANG K, LIU S W, WANG M J, et al., 2018. Formation ages, petrogenesis and geological implications of the archean granitoid rocks in the Xinbin-Weiziyu Area, northern Liaoning province[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 54(1): 61-79. (in Chinese with English abstract)
    WANG M J, LIU S W, WANG W, et al., 2016a. Petrogenesis and tectonic implications of the Neoarchean North Liaoning tonalitic-trondhjemitic gneisses of the North China Craton, North China[J]. Journal of Asian Earth Sciences, 131: 12-39. doi: 10.1016/j.jseaes.2016.09.012
    WANG W, LIU S W, CAWOOD P A, et al., 2016b. Late Neoarchean subduction-related crustal growth in the Northern Liaoning region of the North China Craton: evidence from ~2.55 to 2.50 Ga granitoid gneisses[J]. Precambrian Research, 281: 200-223. doi: 10.1016/j.precamres.2016.05.018
    WARR L N, 2021. IMA-CNMNC approved mineral symbols[J]. Mineralogical Magazine, 85(3): 291-320. doi: 10.1180/mgm.2021.43
    WATSON E B, HARRISON T M, 1984. Accessory minerals and the geochemical evolution of crustal magmatic systems: a summary and prospectus of experimental approaches[J]. Physics of the Earth and Planetary Interiors, 35(1-3): 19-30. doi: 10.1016/0031-9201(84)90031-1
    WEI C J, QIAN J H, ZHOU X W, 2014. Paleoproterozoic crustal evolution of the Hengshan-Wutai-Fuping region, North China craton[J]. Geoscience Frontiers, 5(4): 485-497. doi: 10.1016/j.gsf.2014.02.008
    WEI C J, GUAN X, DONG J, 2017. HT-UHT metamorphism of metabasites and the petrogenesis of TTGs[J]. Acta Petrologica Sinica, 33(5): 1381-1404. (in Chinese with English abstract)
    WHITE R W, POWELL R, HOLLAND T J B, et al., 2000. The effect of TiO2 and Fe2O3 on metapelitic assemblages at greenschist and amphibolite facies conditions: mineral equilibria calculations in the system K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2-Fe2O3[J]. Journal of Metamorphic Geology, 18(5): 497-511. doi: 10.1046/j.1525-1314.2000.00269.x
    WHITE R W, POWELL R, HOLLAND T J B, 2007. Progress relating to calculation of partial melting equilibria for metapelites[J]. Journal of Metamorphic Geology, 25(5): 511-527. doi: 10.1111/j.1525-1314.2007.00711.x
    WHITE R W, POWELL R, HOLLAND T J B, et al., 2014. New mineral activity-composition relations for thermodynamic calculations in metapelitic systems[J]. Journal of Metamorphic Geology, 32(3): 261-286. doi: 10.1111/jmg.12071
    WHITNEY D L, EVANS B W, 2010. Abbreviations for names of rock-forming minerals[J]. American Mineralogist, 95(1): 185-187. doi: 10.2138/am.2010.3371
    WIEDENBECK M, ALLÉ P, CORFU F, et al., 1995. Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses[J]. Geostandards Newsletter, 19(1): 1-23. doi: 10.1111/j.1751-908X.1995.tb00147.x
    WINTHER K T, NEWTON R C, 1991. Experimental melting of hydrous low-K tholeiite: evidence on the origin of Archaean cratons[J]. Bulletin of the Geological Society of Denmark, 39: 213-228. doi: 10.37570/bgsd-1991-39-10
    WU D, WEI C J, 2021. Metamorphic evolution of two types of garnet amphibolite from the Qingyuan terrane, North China Craton: insights from phase equilibria modelling and zircon dating[J]. Precambrian Research, 355: 106091. doi: 10.1016/j.precamres.2021.106091
    WU K K, ZHAO G C, SUN M, et al., 2013. Metamorphism of the northern Liaoning Complex: implications for the tectonic evolution of Neoarchean basement of the Eastern Block, North China Craton[J]. Geoscience Frontiers, 4(3): 305-320. doi: 10.1016/j.gsf.2012.11.005
    WU M L, LIN S F, WAN Y S, et al., 2016. Crustal evolution of the Eastern Block in the North China Craton: constraints from zircon U-Pb geochronology and Lu-Hf isotopes of the northern Liaoning Complex[J]. Precambrian Research, 275: 35-47. doi: 10.1016/j.precamres.2015.12.013
    WYLLIE P J, WOLF M B, 1993. Amphibolite dehydration-melting: sorting out the solidus[J]. Geological Society, London, Special Publications, 76(1): 405-416. doi: 10.1144/GSL.SP.1993.076.01.20
    YANG C, WEI C J., 2017. Two phases of granulite facies metamorphism during Neoarchean and Paleoproterozoic in the East Hebei, North China Craton: records from mafic granulites[J]. Precambrian Research, 2017(301).
    YAKYMCHUK C, BROWN M, 2014. Behaviour of zircon and monazite during crustal melting[J]. Journal of the Geological Society, 171(4): 465-479. doi: 10.1144/jgs2013-115
    YAKYMCHUK C, CLARK C, WHITE R W, 2017. Phase relations, reaction sequences and petrochronology[J]. Reviews in Mineralogy and Geochemistry, 83(1): 13-53. doi: 10.2138/rmg.2017.83.2
    YU C Y, YANG T, ZHANG J, et al., 2022. Coexisting diverse P-T-t paths during Neoarchean Sagduction: Insights from numerical modeling and applications to the eastern North China Craton[J]. Earth and Planetary Science Letters, 586: 117529. doi: 10.1016/j.epsl.2022.117529
    YUAN L L, LIU J, ZHANG X H, et al., 2020. Late Neoarchean magmatism and crustal growth in northern Liaoning: Evidence from zircon U-Pb geochronology and petro-geochemistry of the Qingyuan trondhjemites[J]. Acta Petrologica Sinica, 36(2): 333-355. (in Chinese with English abstract) doi: 10.18654/1000-0569/2020.02.02
    ZHAI M G, YANG R Y, LU W J, et al., 1985. Geochemistry and evolution of the Qingyuan Archaean granite-greenstone terrain, NE China[J]. Precambrian Research, 27(1-3): 37-62. doi: 10.1016/0301-9268(85)90005-1
    ZHAI M G, BIAN A G, ZHAO T P, 2000. The amalgamation of the supercontinent of North China Craton at the end of Neo-Archaean and its breakup during late Palaeoproterozoic and Meso-Proterozoic[J]. Science in China Series D: Earth Sciences, 43(1): 219-232.
    ZHAI M G, GUO J H, LIU W J, 2005. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton: a review[J]. Journal of Asian Earth Sciences, 24(5): 547-561. doi: 10.1016/j.jseaes.2004.01.018
    ZHAI M G, SANTOSH M, 2011. The early Precambrian odyssey of the North China Craton: a synoptic overview[J]. Gondwana Research, 20(10): 6-25.
    ZHAI M G, SANTOSH M, 2013. Metallogeny of the North China Craton: link with secular changes in the evolving Earth[J]. Gondwana Research, 24(1): 275-297. doi: 10.1016/j.gr.2013.02.007
    ZHAI M G, 2019. Tectonic evolution of the north China craton[J]. Journal of Geomechanics, 25(5): 722-745. (in Chinese with English abstract)
    ZHANG H C G, LIU J H, CHEN Y C, et al., 2019. Neoarchean metamorphic evolution and geochronology of the Miyun metamorphic complex, North China Craton[J]. Precambrian Research, 320: 78-92. doi: 10.1016/j.precamres.2018.10.015
    ZHANG Y H, WEI C J, TIAN W, et al., 2013. Reinterpretation of metamorphic age of the Hengshan complex, North China Craton[J]. Chinese Science Bulletin, 58(34): 4300-4307. doi: 10.1007/s11434-013-5993-x
    ZHANG Y Y, WEI C, CHU H, 2020. Paleoproterozoic oceanic subduction in the North China Craton: Insights from the metamorphic P-T-t paths of the Chicheng Mélange in the Hongqiyingzi Complex[J]. Precambrian Research, 342: 105671. doi: 10.1016/j.precamres.2020.105671
    ZHANG Y Y, WEI C J, CHU H, 2021. Multi-phase metamorphism in the northern margin of the North China Craton: Records from metapelite in the Hongqiyingzi Complex[J]. Gondwana Research, 98: 289-308. doi: 10.1016/j.gr.2021.06.012
    ZHAO G, 1995. Metamorphic P-T-t paths of the eastern Hebei, western Shandong, Fuping, Wutai and Hengshan domains, North China Craton[J]. Tectonothermal Evolution of the Basement Rocks in the North China Craton, 11-48.
    ZHAO G C, SUN M, WILDE S A, et al., 2005. Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited[J]. Precambrian Research, 136(2): 177-202. doi: 10.1016/j.precamres.2004.10.002
    ZHAO G C, CAWOOD P A, LI S Z, et al., 2012. Amalgamation of the North China Craton: key issues and discussion[J]. Precambrian Research, 222-223: 55-76.
    ZHENG J P, 2020. Internal and external factors in continental lithosphere mantle replacement in eastern China[J]. Journal of Geomechanics, 26(5): 742-758, doi: 10.12090/j.issn.1006-6616.2020.26.05.061. (in Chinese with English abstract)
    白翔, 刘树文, 阎明, 等, 2014. 抚顺南部早前寒武纪变质岩的地质事件序列[J]. 岩石学报, 30(10): 2905-2924.
    万渝生, 宋彪, 耿元生, 等, 2005a. 辽北抚顺—清原地区太古宙基底地球化学组成特征及其地质意义[J]. 地质论评, 51(2): 128-137. doi: 10.16509/j.georeview.2005.02.003
    万渝生, 宋彪, 杨淳, 等, 2005b. 辽宁抚顺-清原地区太古宙岩石SHRIMP锆石U—Pb年代学及其地质意义[J]. 地质学报, 79(1): 78-87. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200501009.htm
    万渝生, 董春艳, 颉颃强, 等, 2022. 华北克拉通新太古代早期—中太古代晚期(2.6~3.0 Ga)巨量陆壳增生: 综述[J]. 地质力学学报, 28(5): 866-906, doi: 10.12090/j.issn.1006-6616.20222817.
    王康, 刘树文, 王茂江, 等, 2018. 辽北新宾-苇子峪地区太古宙花岗质岩石的形成年代、成因及其地质意义[J]. 北京大学学报(自然科学版), 54(1): 61-79. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201801007.htm
    魏春景, 关晓, 董杰, 2017. 基性岩高温-超高温变质作用与TTG质岩成因[J]. 岩石学报, 33(5): 1381-1404. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201705002.htm
    袁玲玲, 刘洁, 张晓晖, 等, 2020. 辽北新太古代晚期岩浆热事件与陆壳生长: 来自清原奥长花岗岩的锆石U-Pb年代学和岩石地球化学证据[J]. 岩石学报, 36(2): 333-355. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB202002002.htm
    翟明国, 2019. 华北克拉通构造演化[J]. 地质力学学报, 25(5): 722-745. doi: 10.12090/j.issn.1006-6616.2019.25.05.063
    郑建平, 2020. 中国东部大陆岩石圈地幔置换作用的内外原因[J]. 地质力学学报, 26(5): 742-758, doi: 10.12090/j.issn.1006-6616.2020.26.05.061.
  • Relative Articles

    HAN Mingming, CHEN Lichun, ZENG Di, LI Yanbao, LIANG Mingjian, GAO Shuaipo, WANG Dongbing, LUO Liang. 2022: Discussion on the latest surface ruptures near the Zhonggu village along the Selaha segment of the Xianshuihe fault zone. Journal of Geomechanics, 28(6): 969-980. doi: 10.12090/j.issn.1006-6616.20222824
    CHANG Zufeng, ZHANG Jianguo, SHEN Chongyang, LI Chunguang, LIU Changwei, WANG Guangming, YU Jiang. 2022: The 2012 Thabeikkjin (Myanmar) M 7.0 earthquake and its surface rupture characteristics. Journal of Geomechanics, 28(2): 169-181. doi: 10.12090/j.issn.1006-6616.2021161
    HAN Shuai, WU Zhonghai, GAO Yang, LU Haifeng. 2022: Surface rupture investigation of the 2022 Menyuan MS 6.9 Earthquake, Qinghai, China: Implications for the fault behavior of the Lenglongling fault and regional intense earthquake risk. Journal of Geomechanics, 28(2): 155-168. doi: 10.12090/j.issn.1006-6616.2022013
    ZHAO Di, CHEN Peng, LI Rongxi, WU Xiaoli, ZHAO Bangsheng, LIU Qi, WANG Xiaoxue. 2022: Discovery of the surface rupture zone along the southern branch of the Longshoushan Fault Zone, NW China and its significance to the deep structures of the 1954 Shandan MS 7¼ earthquake. Journal of Geomechanics, 28(4): 501-512. doi: 10.12090/j.issn.1006-6616.2022045
    GAI Hailong, YAO Shenghai, YANG Liping, KANG Taibo, YIN Xiang, CHEN Ting, LI Xin. 2021: Characteristics and causes of coseismic surface rupture triggered by the "5.22" MS 7.4 Earthquake in Maduo, Qinghai, and their significance. Journal of Geomechanics, 27(6): 899-912. doi: 10.12090/j.issn.1006-6616.2021.27.06.073
    WANG Dong, WANG Jianfeng, LI Tianbin, ZENG Peng, MA Junjie, CHEN Wei. 2021: Analysis of three-dimensional movement characteristics of rockfall: A case study at a railway tunnel entrance in the southwestern mountainous area, China. Journal of Geomechanics, 27(1): 96-104. doi: 10.12090/j.issn.1006-6616.2021.27.01.010
    HUANG Qiangbing, GAO Huan, LIU Nina, MA Yujie. 2018: SHAKING TABLE MODEL TEST ON SEISMIC RESPONSE OF METRO TUNNEL CROSSING GROUND FISSURE SITE. Journal of Geomechanics, 24(6): 785-794. doi: 10.12090/j.issn.1006-6616.2018.24.06.081
    CHEN Xing, HUANG Qiangbing, LIU Nina, ZHAO Teng. 2018: STUDY ON GROUND SETTLEMENT OF ENGINEERING SITE OF METRO TUNNEL ADJACENT TO GROUND FISSURE ZONE UNDER THE ACTION OF EARTHQUAKE. Journal of Geomechanics, 24(5): 714-722. doi: 10.12090/j.issn.1006-6616.2018.24.05.073
    BAO Linhai, DU Yi, GUO Qiliang, ZHANG Yanshan. 2017: IN-SITU STRESS MEASUREMENT AND RESEARCH ON TECTONIC STRESS FIELD DISTRIBUTION LAW OF CHENGDU-LANZHOU RAILWAY. Journal of Geomechanics, 23(5): 734-742.
    REN Sanshao, GUO Changbao, WU Ruian, SHEN Yaqi, ZHANG Tao. 2017: DEVELOPMENT CHARACTERISTICS AND STABILITY ANALYSIS OF THE HONGHUATUN ANCIENT LANDSLIDE AT SONGPAN TUNNEL ENTRANCE OF CHENGDU-LANZHOU RAILWAY. Journal of Geomechanics, 23(5): 754-765.
    LI Guang-wei, DU Yu-ben, JIANG Liang-wen, GUO Chang-bao, SHEN Wei, LIU Xiao-yi. 2015: RESEARCH ON THE ENGINEERING GEOLOGY CONDITION AND RAILWAY ROUTES COMPARISON ALONG THE Mt. GAOLIGONG SECTION, DALI-RUILI RAILWAY. Journal of Geomechanics, (1): 73-86.
    GUO Chang-bao, ZHANG Yong-shuang, QU Ke, XIONG Tan-yu, FU Xiao-xiao, DU Yu-ben. 2014: QUANTITATIVE EVALUATION OF CRUSTAL STABILITY ALONG THE BAOSHAN-RUILI SECTION OF DALI-RUILI RAILWAY AND ITS ADJACENT REGION. Journal of Geomechanics, 20(1): 70-81.
    WANG Tao, HU Qiu-yun, ZHANG Yong-shuang, WU Shu-ren, XIN Peng. 2014: MULTI-SCALE LANDSLIDE HAZARD ASSESSMENT FOR KEY SECTION OF CHENGDU-LANZHOU RAILWAY, WENCHUAN SEISMIC REGION. Journal of Geomechanics, 20(4): 379-391.
    MA Yin-sheng, ZHANG Yong-shuang, HU Dao-gong, YANG Nong, LONG Chang-xing, HOU Cun-tang, YAN Peng, WU Zhong-hai, YANG Zhen-yu, LEI Wen-zhi, TAN Cheng-xuan. 2010: THE SURFACE RUPTURES AND THE MACROSCOPICAL EPICENTER OF YUSHU MS7.1 EARTHQUAKE. Journal of Geomechanics, 16(2): 115-128.
    GUO Chang-bao, LEI Wei-zhi, ZHANG Yong-shuang, LIU Jing-ru. 2006: MAIN GEOHAZARD TYPES AND THEIR OCCURRENCE CHARACTERISTICS ALONG THE YUNNAN-TIBET RAILWAY IN NW YUNNAN. Journal of Geomechanics, 12(2): 228-235.
    JIANG Wa-li, XIE Xin-sheng. 2006: CHARACTERISTICS OF SEGMENTS OF SURFACE RUPTURES OF STRONG EARTHQUAKES ALONG THE EAST KUNLUN ACTIVE FAULT ZONE. Journal of Geomechanics, 12(2): 132-139.
    PENG Hua, WU Zhen-han, MA Xiu-min. 2006: UNMANNED IN-SITU STRESS MONITORING STATIONS ALONG THE QINGHAI-TIBET RAILWAY. Journal of Geomechanics, 12(1): 96-104.
    QING San-hui, HUANG Run-qiu, LI Dong, JIANG Liang-wen. 2006: RAILWAY LOCATION IN A MOUNTAINOUS ENVIRONMENT IN AREAS OF ACTIVE STRUCTURES. Journal of Geomechanics, 12(2): 243-251.
    OUYANG Yong-long, HU Dao-gong, WANG Lian-jie, ZHANG You, CHEN Xin-long. 2005: FINITE ELEMENT ANALYSIS OF EFFECTS OF STICK-SLIP MOVEMENT OF THE SEISMOGENIC FAULT ON THE DEFORMATION OF THE QINGHAI-TIBET RAILWAY——A CASE STUDY OF THE EAST KUNLUN ACTIVE FAULT. Journal of Geomechanics, 11(4): 377-385.
    LI Jin-suo, PENG Hua, Cui Wei, MA Xiu-min, YANG Shao-xi, LIAO Jian-she. 2005: RESULTS OF ROCK STRESS MEASUREMENTS AND ENGINEERING APPLICATION OF A RAILWAY TUNNEL IN NORTHWESTERN YUNNAN. Journal of Geomechanics, 11(2): 135-144.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-052024-062024-072024-082024-092024-102024-112024-122025-012025-022025-032025-040102030405060
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 16.2 %FULLTEXT: 16.2 %META: 78.5 %META: 78.5 %PDF: 5.3 %PDF: 5.3 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 4.9 %其他: 4.9 %其他: 0.1 %其他: 0.1 %Sacramento: 0.4 %Sacramento: 0.4 %三明: 0.1 %三明: 0.1 %上海: 0.6 %上海: 0.6 %上饶: 0.9 %上饶: 0.9 %中卫: 2.5 %中卫: 2.5 %乌鲁木齐: 0.3 %乌鲁木齐: 0.3 %信阳: 0.1 %信阳: 0.1 %北京: 16.1 %北京: 16.1 %北海: 0.4 %北海: 0.4 %十堰: 0.1 %十堰: 0.1 %南京: 0.5 %南京: 0.5 %南宁: 0.1 %南宁: 0.1 %南昌: 0.3 %南昌: 0.3 %南通: 0.1 %南通: 0.1 %古吉拉特: 0.1 %古吉拉特: 0.1 %吉林: 0.1 %吉林: 0.1 %呼和浩特: 0.1 %呼和浩特: 0.1 %哈尔滨: 0.4 %哈尔滨: 0.4 %哥伦布: 0.4 %哥伦布: 0.4 %四平: 0.1 %四平: 0.1 %大同: 1.5 %大同: 1.5 %大庆: 0.1 %大庆: 0.1 %天津: 0.9 %天津: 0.9 %太原: 0.1 %太原: 0.1 %安阳: 0.1 %安阳: 0.1 %宝鸡: 0.1 %宝鸡: 0.1 %宣城: 0.5 %宣城: 0.5 %屯昌: 0.1 %屯昌: 0.1 %巴音郭楞: 0.1 %巴音郭楞: 0.1 %广州: 0.8 %广州: 0.8 %库比蒂诺: 0.8 %库比蒂诺: 0.8 %廊坊: 0.1 %廊坊: 0.1 %张家口: 5.3 %张家口: 5.3 %徐州: 0.3 %徐州: 0.3 %成都: 0.4 %成都: 0.4 %扬州: 0.1 %扬州: 0.1 %抚顺: 0.1 %抚顺: 0.1 %拉萨: 0.1 %拉萨: 0.1 %无锡: 0.1 %无锡: 0.1 %昆明: 0.4 %昆明: 0.4 %朔州: 0.1 %朔州: 0.1 %朝阳: 0.1 %朝阳: 0.1 %本溪: 0.1 %本溪: 0.1 %杭州: 1.1 %杭州: 1.1 %枣庄: 0.1 %枣庄: 0.1 %株洲: 0.1 %株洲: 0.1 %格兰特县: 0.9 %格兰特县: 0.9 %武汉: 1.5 %武汉: 1.5 %沈阳: 0.3 %沈阳: 0.3 %济南: 0.5 %济南: 0.5 %济源: 0.1 %济源: 0.1 %海口: 0.9 %海口: 0.9 %温州: 0.1 %温州: 0.1 %湖州: 0.3 %湖州: 0.3 %漯河: 0.6 %漯河: 0.6 %漳州: 0.1 %漳州: 0.1 %玉林: 0.1 %玉林: 0.1 %石家庄: 1.3 %石家庄: 1.3 %绵阳: 0.5 %绵阳: 0.5 %芒廷维尤: 11.1 %芒廷维尤: 11.1 %芝加哥: 1.9 %芝加哥: 1.9 %苏州: 0.3 %苏州: 0.3 %莫斯科: 0.1 %莫斯科: 0.1 %莱芜: 0.1 %莱芜: 0.1 %西宁: 17.1 %西宁: 17.1 %西安: 0.8 %西安: 0.8 %西雅图: 0.4 %西雅图: 0.4 %诺沃克: 13.0 %诺沃克: 13.0 %贵阳: 0.5 %贵阳: 0.5 %费利蒙: 0.4 %费利蒙: 0.4 %赣州: 0.4 %赣州: 0.4 %运城: 2.0 %运城: 2.0 %邯郸: 0.1 %邯郸: 0.1 %郑州: 0.4 %郑州: 0.4 %重庆: 0.4 %重庆: 0.4 %银川: 0.1 %银川: 0.1 %长春: 0.1 %长春: 0.1 %长沙: 0.4 %长沙: 0.4 %防城港: 0.1 %防城港: 0.1 %阳泉: 0.1 %阳泉: 0.1 %青岛: 0.3 %青岛: 0.3 %黄冈: 0.1 %黄冈: 0.1 %齐齐哈尔: 0.1 %齐齐哈尔: 0.1 %其他其他Sacramento三明上海上饶中卫乌鲁木齐信阳北京北海十堰南京南宁南昌南通古吉拉特吉林呼和浩特哈尔滨哥伦布四平大同大庆天津太原安阳宝鸡宣城屯昌巴音郭楞广州库比蒂诺廊坊张家口徐州成都扬州抚顺拉萨无锡昆明朔州朝阳本溪杭州枣庄株洲格兰特县武汉沈阳济南济源海口温州湖州漯河漳州玉林石家庄绵阳芒廷维尤芝加哥苏州莫斯科莱芜西宁西安西雅图诺沃克贵阳费利蒙赣州运城邯郸郑州重庆银川长春长沙防城港阳泉青岛黄冈齐齐哈尔

Catalog

    Figures(9)  / Tables(4)

    Article Metrics

    Article views (776) PDF downloads(81) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return