高压超高压变泥质岩适用的地质温压计评述
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摘要
高压超高压变泥质岩形成温压条件及p-T演化轨迹是高压超高压变质作用研究的重要内容。本文介绍了高压超高压变泥质岩适用的几种地质温压计,包括石榴子石-多硅白云母Fe~(2+)-Mg交换温度计、石榴子石-绿泥石Fe~(2+)-Mg交换温度计、硬绿泥石-绿泥石Fe~(2+)-Mg交换温度计、多硅白云母Si含量压力计、金红石Zr含量温度计、榍石Zr含量温压计、锆石Ti含量温度计、石英Ti含量温度计以及氧同位素温度计,并对上述温压计的适用条件及使用时的注意事项做了简要评述。
p-T conditions and p-T paths of(ultra) high-pressure metapelites are important aspects in the study of(ultra) high-pressure metamorphism. This paper introduces several kinds of geothermobarometers applicable to(ultra) high-pressure metapelites, which include the garnet-phengite Fe~(2+)-Mg exchange geothermometer, garnet-chlorite Fe~(2+)-Mg exchange geothermometer, chloritoid-chlorite Fe~(2+)-Mg exchange geothermometer, Si-in-phengite geobarometer, Zr-in-rutile geothermometer, Zr-in-titanite geothermobarometer, Ti-in-zircon geothermobarometer, Tiin-quartz geothermobarometer and oxygen isotope geothermometer. In addition, a review is given concerning the applicable conditions and points for attention in use of the above geothermobarometers.
p-T conditions and p-T paths of(ultra) high-pressure metapelites are important aspects in the study of(ultra) high-pressure metamorphism. This paper introduces several kinds of geothermobarometers applicable to(ultra) high-pressure metapelites, which include the garnet-phengite Fe~(2+)-Mg exchange geothermometer, garnet-chlorite Fe~(2+)-Mg exchange geothermometer, chloritoid-chlorite Fe~(2+)-Mg exchange geothermometer, Si-in-phengite geobarometer, Zr-in-rutile geothermometer, Zr-in-titanite geothermobarometer, Ti-in-zircon geothermobarometer, Tiin-quartz geothermobarometer and oxygen isotope geothermometer. In addition, a review is given concerning the applicable conditions and points for attention in use of the above geothermobarometers.
引文
Ashley K T,Webb L E,Spear F S,et al.2013.P-T-D histories from quartz:A case study of the application of the Titani Q thermobarometer to progressive fabric development in metapelites[J].Geochemistry Geophysics Geosystems,14(9):3 821~3 843.
Ashworth J R and Evirgen M M.1984.Mineral chemistry of regional chloritoid assemblages in the Chlorite Zone,Lycian Nappes,South-west Turkey[J].Mineralogical Magazine,48(237):159~165.
Balen D E,Horváth P,Finger F,et al.2013.Phase equilibrium,geothermobarometric and xenotime age dating constraints on the Alpine metamorphism recorded in chloritoid schists from the southern part of the Tisia Mega-Unit(Slavonian Mts.,NE Croatia)[J].Int.J.Earth Sci.(Geol.Rundsch),102(4):1 091~1 109.
Chen Yan,Wei Chunjing,Zhang Jingsen,et al.2005.Phase equilibria of mica-schists and gneisses in the HP-UHP belt of Southern Dabie Shan[J].Acta Petrologica Sinica,21(6):1 657~1 668(in Chinese with English abstract).
Chen Zhenyu,Yu Jinjie,Li Xiaofeng,et al.2007.Discussion of the application of Zr-in-Rutile thermometer in the Sulu-Dabie UHP eclogites[J].Acta Geologica Sinica,81(10):1 369~1 377(in Chinese with Ehglish abstract).
Cherniak D J,Watson E B and Wark D A.2007.Ti diffusion in quartz[J].Chemical Geology,236(1~2):65~74.
Chiba H,Chacko T,Clayton R N,et al.1989.Oxygen isotope fractionations involving diopside,forsterite,magnetite,and calcite:Application to geothermometry[J].Geochimica et Cosmochimica Acta,53(11):2 985~2 995.
Clayton R N,Goldsmith J R and Mayeda T K.1989.Oxygen isotope fractionation in quartz,albite,anorthite and calcite[J].Geochimica et Cosmochimica Acta,53(3):725~733.
Coggon R and Holland T.2002.Mixing properties of phengitic micas and revised garnet-phengite thermobarometers[J].Journal of Metamorphic Geology,20(7):683~696.
Collings D,Savov I,Maneiro K,et al.2016.Late Cretaceous UHP metamorphism recorded in kyanite-garnet schists from the Central Rhodope Mountains,Bulgaria[J].Lithos,s 246~247:165~181.
Degeling H S.2002.Zircon Equilibria in Metamorphic Rocks[D].The Australian National University.
Dickinson M P and Hewitt D A.1986.A garnet-chlorite geothermometer(abstract)[J].Geological Society of America Abstracts with Programs,18:584.
Du J X,Zhang L F,Bader T,et al.2014.Metamorphic evolution of ultrahigh-pressure rocks from Chinese Southwestern Tianshan and a possible indicator of UHP metamorphism using garnet composition in lowT eclogites[J].Journal of Asian Earth Sciences,91(3):69~88.
Ewing T A,Hermann J R and Rubatto D.2013.The robustness of the Zrin-rutile and Ti-in-zircon thermometers during high-temperature metamorphism(Ivrea-Verbano Zone,northern Italy)[J].Contributions to Mineralogy and Petrology,165(4):757~779.
Ferry J M and Watson E B.2007.New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers[J].Contributions to Mineralogy and Petrology,154(4):429~437.
Ghent E D,Stout M Z,Black P M,et al.1987.Chloritoid-bearing rocks associated with blueschists and eclogites,northern New Caledonia[J].Journal of Metamorphic Geology,5(2):239~254.
Grambling J A.1990.Internally-consistent geothermometry and H2O barometry in metamorphic rocks:The example garnet-chlorite-quartz[J].Contributions to Mineralogy and Petrology,105(6):617~628.
Green T H and Hellman P L.1982.Fe-Mg partitioning between coexisting garnet and phengite at high pressure,and comments on a garnetphengite geothermometer[J].Lithos,15(4):253~266.
Guidotti C V,Yates M G,Dyar M D,et al.1994.Petrogenetic implications of the Fe(super 3+)content of muscovite in pelitic schists[J].American Mineralogist,79(7~8):793~795.
Hayden L A,Watson E B and Wark D A.2008.A thermobarometer for sphene(titanite)[J].Contributions to Mineralogy and Petrology,155(4):529~540.
Huang R and Audétat A.2012.The titanium-in-quartz(Titani Q)thermobarometer:A critical examination and re-calibration[J].Geochimica et Cosmochimica Acta,84:75~89.
Hynes A and Forest R C.1988.Empirical garnet-muscovite geothermometry in low-grade metapelites,Selwyn Range(Canadian Rockies)[J].Journal of Metamorphic Geology,6(3):297~309.
Kouketsu Y,Enami M and Mizukami T.2010.Omphacite-bearing metapelite from the Besshi region,Sambagawa metamorphic belt,Japan:Prograde eclogite facies metamorphism recorded in metasediment[J].Journal of Mineralogical and Petrological Sciences,105(1):9~19.
Krogh E J and Rheim A.1978.Temperature and pressure dependence of Fe-Mg partitioning between garnet and phengite,with particular reference to eclogites[J].Contributions to Mineralogy and Petrology,66(1):75~80.
Liou J G,Ernst W G,Zhang R Y,et al.2009.Ultrahigh-pressure minerals and metamorphic terranes:The view from China[J].Journal of Asian Earth Sciences,35(3~4):199~231.
Liu Xiaochun,Lou Yuxing and Dong Shuwen.2005.P-T path of lowtemperature eclogites from the Tongbaishan area[J].Acta Petrologica Sinica,21(4):1 081~1 093(in Chinese with English abstract).
Liu Yican,Deng Liangpeng,Gu Xiaofeng,et al.2015.Application of Ti-in-zircon and Zr-in-rutile thermometers to constrain high-temperature metamorphism in eclogites from the Dabie orogen,central China[J].Gondwana Research,27(1):410~423.
LüZ,Bucher K,Zhang L F,et al.2012.The Habutengsu metapelites and metagreywackes in western Tianshan,China:Metamorphic evolution and tectonic implications[J].Journal of Forensic Sciences,57(6):907~926.
LüZeng and Zhang Lifei.2016.Differential evolution of high-pressure and ultrahigh-pressure metapelites from Habutengsu,Chinese Western Tianshan:Phase equilibria modelling and40Ar/39Ar geochronology[J].Acta Geologica Sinica(English Edition),90(2):628~640.
LüZeng,Zhang Lifei,Qu Junfeng,et al.2007.Prtrology and metamorphic P-T path of eclogites from Habutengsu,southwestern Tianshan,Xinjiang[J].Acta Petrologica Sinica,23(7):1 617~1 626(in Chinese with English abstract).
Maldonado R,Ortega-Gutiérrez F and Hernández D.2016.Garnet-chloritoid-paragonite metapelite from the Chuacús Complex(Central Guatemala):New evidence for continental subduction in the North America-Caribbean plate boundary[J].European Journal of Mineralogy,28:1 169~1 186.
Massonne H J,Opitz J,Theye T,et al.2013.Evolution of a very deeply subducted metasediment from As Sifah,northeastern coast of Oman[J].Lithos,s156~159(1):171~185.
Massonne H J and Schreyer W.1987.Phengite geobarometry based on the limiting assemblage with K-feldspar,phlogopite,and quartz[J].Contributions to Mineralogy and Petrology,96(2):212~224.
Massonne H J and Schreyer W.1989.Stability field of the high-pressure assemblage Talc+Phengite and 2 new phengite barometers[J].European Journal of Mineralogy,1(3):391~410.
Massonne H J and Szpurka Z.1997.Thermodynamic properties of white micas on the basis of high-pressure experiments in the systems K2O-Mg O-Al2O3-Si O2-H2O and K2O-Fe O-Al2O3-Si O2-H2O[J].Lithos,41(1~3):229~250.
Matthews A.1994.Oxygen isotope geothermometers for metamorphic rocks[J].Journal of Metamorphic Geology,12(12):211~219.
Matthews A,Goldsmith J R and Clayton R N.1983.Oxygen isotope fractionations involving pyroxenes:The calibration of mineral-pair geothermometers[J].Geochimica et Cosmochimica Acta,47(3):631~644.
Min K and Cho M.1998.Metamorphic evolution of the northwestern Ogcheon metamorphic belt,South Korea[J].Lithos,43(1):31~51.
Mitchell R J and Harley S L.2017.Zr-in-rutile resetting in aluminosilicate bearing ultra-high temperature granulites:Refining the record of cooling and hydration in the Napier Complex,Antarctica[J].Lithos,272~273:128~146.
Moazzen M.2004.Chlorite-chloritoid-garnet equilibria and geothermometry in the Sanandaj-Sirjan metamorphic belt,Southern Iran[J].Iranian Journal of Science and Technolagy,28(A1):65~78.
Nachlas W O,Whitney D L,Teyssier C,et al.2014.Titanium concentration in quartz as a record of multiple deformation mechanisms in an extensional shear zone[J].Geochemistry Geophysics Geosystems,15(4):1 374~1 397.
O'Brien P J and Tzler J R.2003.High-pressure granulites:formation,recovery of peak conditions and implications for tectonics[J].Journal of Metamorphic Geology,21(1):3~20.
zdamar S F,Roden M,Esenli F,et al.2012.Geochemical features and K-Ar age data from metadetrital rocks and high-K metasomatized metarhyolites in the Afyon-BolkardaZone(Ilgin-Konya),SW Turkey[J].Neues Jahrbuch für Mineralogie-Abhandlungen,189(2):155~176.
Pape J,Mezger K and Robyr M.2016.A systematic evaluation of the Zrin-rutile thermometer in ultra-high temperature(UHT)rocks[J].Contributions to Mineralogy and Petrology,171(5):1~20.
Powell R and Holland T J B.2008.On thermobarometry[J].Journal of Metamorphic Geology,26(2):155~179.
Ren Y F,Chen D L,Hauzenberger C,et al.2016.Petrology and geochronology of ultrahigh-pressure granitic gneiss from South Dulan,North Qaidam belt,NW China[J].International Geology Review,58(2):171~195.
Saki A,Moazzen M and Oberhnsli R.2012.Mineral chemistry and thermobarometry of the staurolite-chloritoid schists from Poshtuk,NWIran[J].Geological Magazine,149(6):1 077~1 088.
engün F.2017.Zr-in-rutile thermometry of eclogites from the Karakaya Complex in NW Turkey:Implications for rutile growth during subduction zone metamorphism[J].Chemie der Erde-Geochemistry,77(1):95~104.
Shatsky V S,Skuzovatov S Y,Ragozin A L,et al.2015.Mobility of elements in a continental subduction zone:Evidence from the UHP metamorphic complex of the Kokchetav massif[J].Russian Geology&Geophysics,56(7):1 016~1 034.
Shen Qihan.2009.The recommendation of a systematic list of mineral abbreviations[J].Acta Petrologica et Mineralogica,28(5):495~500(in Chinese with English abstract).
Song S G,Zhang L F,Niu Y L,et al.2007.Eclogite and carpholitebearing metasedimentary rocks in the North Qilian suture zone,NWChina:Implications for Early Palaeozoic cold oceanic subduction and water transport into mantle[J].Journal of Metamorphic Geology,25(5):547~563.
Spear F S,Wark D A,Cheney J T,et al.2006.Zr-in-rutile thermometry in blueschists from Sifnos,Greece[J].Contributions to Mineralogy and Petrology,152(3):375~385.
Stepanov A S,Daniela R,Joerg H,et al.2016.Contrasting P-T paths within the Barchi-Kol UHP terrain(Kokchetav Complex):Implications for subduction and exhumation of continental crust[J].American Mineralogist,101(4):788~807.
Tenczer V and Stüwe K.2003.The metamorphic field gradient in the eclogite type locality,Koralpe region,Eastern Alps[J].Journal of Metamorphic Geology,21(4):377~393.
Thomas J B,Watson E B,Spear F S,et al.2010.Titani Q under pressure:The effect of pressure and temperature on the solubility of Ti in quartz[J].Contributions to Mineralogy and Petrology,160(5):743~759.
Thomas J B,Watson E B,Spear F S,et al.2015.Titani Q recrystallized:Experimental confirmation of the original Ti-in-quartz calibrations[J].Contributions to Mineralogy and Petrology,169(3):1~16.
Tomkins H S,Powell R and Ellis D J.2007.The pressure dependence of the zirconium-in-rutile thermometer[J].Journal of Metamorphic Geology,25(6):703~713.
Ukar E and Cloos M.2016.Graphite-schist blocks in the Franciscan Mélange,San Simeon,California:Evidence of high-P metamorphism[J].Journal of Metamorphic Geology,34(3):191~208.
Vidal O,GofféB,Bousquet R,et al.1999.Calibration and testing of an empirical chloritoid-chlorite Mg-Fe exchange thermometer and thermodynamic data for daphnite[J].Journal of Metamorphic Geology,17(1):25~39.
Wark D A and Watson E B.2006.Titani Q:a titanium-in-quartz geothermometer[J].Contributions to Mineralogy and Petrology,152(6):743~754.
Watson E B and Harrison T M.2005.Zircon thermometer reveals minimum melting conditions on earliest Earth[J].Science,308(5 723):841~844.
Watson E B,Wark D A and Thomas J B,2006.Crystallization thermometers for zircon and rutile[J].Contributions to Mineralogy and Petrology,151(4):413~433.
Wei Chunjing.2011.Approaches and advancement of the study of metamorphic p-T-t paths[J].Earth Science Frontiers,18(2):1~16(in Chinese with English abstract).
Wei C J and Powell R.2003.Phase relations in high-pressure metapelites in the system KFMASH(K2O-Fe O-Mg O-Al2O3-Si O2-H2O)with application to natural rocks[J].Contributions to Mineralogy and Petrology,145(3):301~315.
Wei C J,Qian J H and Tian Z L.2013.Metamorphic evolution of medium-temperature ultra-high pressure(MT-UHP)eclogites from the South Dabie orogen,Central China:an insight from phase equilibria modelling[J].Journal of Metamorphic Geology,31(7):755~774.
Wei C J and Song S G.2010.Chloritoid-glaucophane schist in the North Qilian orogen,NW China:Phase equilibria and P-T path from garnet zonation[J].Journal of Metamorphic Geology,26(3):301~316.
Wei Chunjing,Su Xiangli,Lou Yuxing,et al.2009.A new interpretation of the conventional thermobnbarometry in eclogites:Evidence from the calculated PT pseudosections[J].Acta Petrologica Sinica.25(9):2 078~2 088(in Chinese with English abstract).
Wei C J,Yang Y,Su X L,et al.2009.Metamorphic evolution of lowTeclogite from the North Qilian orogen,NW China:Evidence from petrology and calculated phase equilibria in the system NCKFMASHO[J].Journal of Metamorphic Geology,27(1):55~70.
Whitney D L and Evans B W.2010.Abbreviations for names of rockforming minerals[J].American Mineralogist,95(1):185~187.
Wu Jialin,Zhai Mingguo,Zhang Hong,et al.2015.A brief review of the advance of pseudosection thermobarometry[J].Acta Petrologica Sinica,31(6):1 711~1 721(in Chinese with English abstract).
Wu Yuanbao,Chen Daogong,Xia Qunke,et al.2002.In-situ trace element analyses of zircons from Dabieshan Huangzhen eclogite:Trace element characteristics of eclogite-facies metamorphic zircon[J].Chinese Science Bulletin(in English),47(16):1 398~1 401.
You Zhendong.2007.Ultrahigh presure metamorphism:A new hot spot in earth science[J].Chinese Journal of Nature,29(5):255~264,311~312(in Chinese with English abstract).
YüXiaoning,Song Shuguang,Wei Chunjing,et al.2009.Mg-carpholite metapelite and its implications for ancient oceanic subduction in the North Qilian suture zone,NW China[J].Acta Scientiarum Naturalium Universitatis Pekinensis.45(3):472~480(in Chinese with English abstract).
Zack T and Luvizottow G L.2006.Application of rutile thermometry to eclogites[J].Mineralogy and Petrology,88(1):69~85.
Zack T,Moraes R and Kronz A.2004.Temperature dependence of Zr in rutile:empirical calibration of a rutile thermometer[J].Contributions to Mineralogy and Petrology,148(4):471~488.
Zhang Hongfei and Gao Shan.2012.Geochemistry[M].Beijing:Geological Publishing House(in Chinese).
Zhang L F,Du J X,LüZ,et al.2013.A huge oceanic-type UHP metamorphic belt in southwestern Tianshan,China:Peak metamorphic age and p-T path[J].Chinese Science Bulletin,58(35):4 378~4 383.
Zheng Yongfei.1999.Oxygen isotope fractionation in carbonate and sulfate minerals[J].Geochemical Journal,33(2):109~126.
Zheng Yongfei and Chen Jiangfeng.2000.Stable Isotope Geochemistry[M].Beijing:Science Press(in Chinese).
Zheng Yongfei,Gao Xiaoying,Chen Renxu,et al.2011.Zr-in-rutile thermometry of eclogite in the Dabie orogen:Constraints on rutile growth during continental subduction-zone metamorphism[J].Journal of Asian Earth Sciences,40(2):427~451.
Zheng Yongfei and Simon K.1991.Oxygen isotope fractionation in hematite and magnetite:A theoretical calculation and application to geothermometry of metamorphic iron-formations[J].European Journal of Mineralogy,3(5):877~886.
Zheng Yongfei and Zhao Zifu.2011.Element and isotope equilibration between minerals:Thermodynamic and kinetic controls of geothermometry and isochron dating[J].Acta Petrologica Sinica,27(2):345~364(in chinese with English abstract).
陈振宇,余金杰,李晓峰,等.2007.金红石Zr温度计在苏鲁-大别榴辉岩研究中的应用:问题讨论[J].地质学报,81(10):1 369~1 377.
陈燕,魏春景,张景森,等.2005.大别山南部高压-超高压变质地体中云母片岩和片麻岩的相平衡研究[J].岩石学报,21(6):151~162.
刘晓春,娄玉行,董树文.2005.桐柏山地区低温榴辉岩变质作用的p-T轨迹[J].岩石学报,21(4):1 081~1 093.
吕增,张立飞,曲军锋,等.2007.新疆西南天山哈布腾苏一带榴辉岩的岩石学特征及变质作用p-T轨迹[J].岩石学报,23(7):1 617~1 626.
沈其韩.2009.推荐一个系统的矿物缩写表[J].岩石矿物学杂志,28(5):495~500.
魏春景.2011.变质作用p-T-t轨迹的研究方法与进展[J].地学前缘,18(2):1~16.
魏春景,苏香丽,娄玉行,等.2009.榴辉岩中传统地质温压计新解:来自PT视剖面图的证据[J].岩石学报,25(9):2 078~2 088.
吴佳林,翟明国,张红,等.2015.视剖面图温压计研究进展评述[J].岩石学报,31(6):1 711~1 721.
吴元保,陈道公,夏群科,等.2002.大别山黄镇榴辉岩锆石的微区微量元素分析:榴辉岩相变质锆石的微量元素特征[J].科学通报,47(11):859~863.
杨蔚,林杨挺,郝佳龙,等.2013.亚微米尺度锆石微量元素分布:对锆石Ti温度计的制约[A].中国矿物岩石地球化学学会学术年会[C].
游振东.2007.超高压变质作用:地球科学的新热点[J].自然杂志,29(5):255~264,311~312.
于孝宁,宋述光,魏春景,等.2009.北祁连山含镁纤柱石高压泥质岩及其对古大洋俯冲的意义[J].北京大学学报(自然科学版),45(3):472~480.
张宏飞,高山.2012.地球化学[M].北京:地质出版社.
张立飞,杜瑾雪,吕增,等.2013.新疆西南天山超高压变质带的空间分布、峰期变质时代和p-T轨迹特征[J].科学通报,58(22):2 107~2 112.
郑永飞,陈江峰.2000.稳定同位素地球化学[M].北京:科学出版社.
郑永飞,赵子福.2011.矿物之间的元素和同位素平衡:地质测温和等时线定年的热力学和动力学控制[J].岩石学报,27(2):345~364.
Ashworth J R and Evirgen M M.1984.Mineral chemistry of regional chloritoid assemblages in the Chlorite Zone,Lycian Nappes,South-west Turkey[J].Mineralogical Magazine,48(237):159~165.
Balen D E,Horváth P,Finger F,et al.2013.Phase equilibrium,geothermobarometric and xenotime age dating constraints on the Alpine metamorphism recorded in chloritoid schists from the southern part of the Tisia Mega-Unit(Slavonian Mts.,NE Croatia)[J].Int.J.Earth Sci.(Geol.Rundsch),102(4):1 091~1 109.
Chen Yan,Wei Chunjing,Zhang Jingsen,et al.2005.Phase equilibria of mica-schists and gneisses in the HP-UHP belt of Southern Dabie Shan[J].Acta Petrologica Sinica,21(6):1 657~1 668(in Chinese with English abstract).
Chen Zhenyu,Yu Jinjie,Li Xiaofeng,et al.2007.Discussion of the application of Zr-in-Rutile thermometer in the Sulu-Dabie UHP eclogites[J].Acta Geologica Sinica,81(10):1 369~1 377(in Chinese with Ehglish abstract).
Cherniak D J,Watson E B and Wark D A.2007.Ti diffusion in quartz[J].Chemical Geology,236(1~2):65~74.
Chiba H,Chacko T,Clayton R N,et al.1989.Oxygen isotope fractionations involving diopside,forsterite,magnetite,and calcite:Application to geothermometry[J].Geochimica et Cosmochimica Acta,53(11):2 985~2 995.
Clayton R N,Goldsmith J R and Mayeda T K.1989.Oxygen isotope fractionation in quartz,albite,anorthite and calcite[J].Geochimica et Cosmochimica Acta,53(3):725~733.
Coggon R and Holland T.2002.Mixing properties of phengitic micas and revised garnet-phengite thermobarometers[J].Journal of Metamorphic Geology,20(7):683~696.
Collings D,Savov I,Maneiro K,et al.2016.Late Cretaceous UHP metamorphism recorded in kyanite-garnet schists from the Central Rhodope Mountains,Bulgaria[J].Lithos,s 246~247:165~181.
Degeling H S.2002.Zircon Equilibria in Metamorphic Rocks[D].The Australian National University.
Dickinson M P and Hewitt D A.1986.A garnet-chlorite geothermometer(abstract)[J].Geological Society of America Abstracts with Programs,18:584.
Du J X,Zhang L F,Bader T,et al.2014.Metamorphic evolution of ultrahigh-pressure rocks from Chinese Southwestern Tianshan and a possible indicator of UHP metamorphism using garnet composition in lowT eclogites[J].Journal of Asian Earth Sciences,91(3):69~88.
Ewing T A,Hermann J R and Rubatto D.2013.The robustness of the Zrin-rutile and Ti-in-zircon thermometers during high-temperature metamorphism(Ivrea-Verbano Zone,northern Italy)[J].Contributions to Mineralogy and Petrology,165(4):757~779.
Ferry J M and Watson E B.2007.New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers[J].Contributions to Mineralogy and Petrology,154(4):429~437.
Ghent E D,Stout M Z,Black P M,et al.1987.Chloritoid-bearing rocks associated with blueschists and eclogites,northern New Caledonia[J].Journal of Metamorphic Geology,5(2):239~254.
Grambling J A.1990.Internally-consistent geothermometry and H2O barometry in metamorphic rocks:The example garnet-chlorite-quartz[J].Contributions to Mineralogy and Petrology,105(6):617~628.
Green T H and Hellman P L.1982.Fe-Mg partitioning between coexisting garnet and phengite at high pressure,and comments on a garnetphengite geothermometer[J].Lithos,15(4):253~266.
Guidotti C V,Yates M G,Dyar M D,et al.1994.Petrogenetic implications of the Fe(super 3+)content of muscovite in pelitic schists[J].American Mineralogist,79(7~8):793~795.
Hayden L A,Watson E B and Wark D A.2008.A thermobarometer for sphene(titanite)[J].Contributions to Mineralogy and Petrology,155(4):529~540.
Huang R and Audétat A.2012.The titanium-in-quartz(Titani Q)thermobarometer:A critical examination and re-calibration[J].Geochimica et Cosmochimica Acta,84:75~89.
Hynes A and Forest R C.1988.Empirical garnet-muscovite geothermometry in low-grade metapelites,Selwyn Range(Canadian Rockies)[J].Journal of Metamorphic Geology,6(3):297~309.
Kouketsu Y,Enami M and Mizukami T.2010.Omphacite-bearing metapelite from the Besshi region,Sambagawa metamorphic belt,Japan:Prograde eclogite facies metamorphism recorded in metasediment[J].Journal of Mineralogical and Petrological Sciences,105(1):9~19.
Krogh E J and Rheim A.1978.Temperature and pressure dependence of Fe-Mg partitioning between garnet and phengite,with particular reference to eclogites[J].Contributions to Mineralogy and Petrology,66(1):75~80.
Liou J G,Ernst W G,Zhang R Y,et al.2009.Ultrahigh-pressure minerals and metamorphic terranes:The view from China[J].Journal of Asian Earth Sciences,35(3~4):199~231.
Liu Xiaochun,Lou Yuxing and Dong Shuwen.2005.P-T path of lowtemperature eclogites from the Tongbaishan area[J].Acta Petrologica Sinica,21(4):1 081~1 093(in Chinese with English abstract).
Liu Yican,Deng Liangpeng,Gu Xiaofeng,et al.2015.Application of Ti-in-zircon and Zr-in-rutile thermometers to constrain high-temperature metamorphism in eclogites from the Dabie orogen,central China[J].Gondwana Research,27(1):410~423.
LüZ,Bucher K,Zhang L F,et al.2012.The Habutengsu metapelites and metagreywackes in western Tianshan,China:Metamorphic evolution and tectonic implications[J].Journal of Forensic Sciences,57(6):907~926.
LüZeng and Zhang Lifei.2016.Differential evolution of high-pressure and ultrahigh-pressure metapelites from Habutengsu,Chinese Western Tianshan:Phase equilibria modelling and40Ar/39Ar geochronology[J].Acta Geologica Sinica(English Edition),90(2):628~640.
LüZeng,Zhang Lifei,Qu Junfeng,et al.2007.Prtrology and metamorphic P-T path of eclogites from Habutengsu,southwestern Tianshan,Xinjiang[J].Acta Petrologica Sinica,23(7):1 617~1 626(in Chinese with English abstract).
Maldonado R,Ortega-Gutiérrez F and Hernández D.2016.Garnet-chloritoid-paragonite metapelite from the Chuacús Complex(Central Guatemala):New evidence for continental subduction in the North America-Caribbean plate boundary[J].European Journal of Mineralogy,28:1 169~1 186.
Massonne H J,Opitz J,Theye T,et al.2013.Evolution of a very deeply subducted metasediment from As Sifah,northeastern coast of Oman[J].Lithos,s156~159(1):171~185.
Massonne H J and Schreyer W.1987.Phengite geobarometry based on the limiting assemblage with K-feldspar,phlogopite,and quartz[J].Contributions to Mineralogy and Petrology,96(2):212~224.
Massonne H J and Schreyer W.1989.Stability field of the high-pressure assemblage Talc+Phengite and 2 new phengite barometers[J].European Journal of Mineralogy,1(3):391~410.
Massonne H J and Szpurka Z.1997.Thermodynamic properties of white micas on the basis of high-pressure experiments in the systems K2O-Mg O-Al2O3-Si O2-H2O and K2O-Fe O-Al2O3-Si O2-H2O[J].Lithos,41(1~3):229~250.
Matthews A.1994.Oxygen isotope geothermometers for metamorphic rocks[J].Journal of Metamorphic Geology,12(12):211~219.
Matthews A,Goldsmith J R and Clayton R N.1983.Oxygen isotope fractionations involving pyroxenes:The calibration of mineral-pair geothermometers[J].Geochimica et Cosmochimica Acta,47(3):631~644.
Min K and Cho M.1998.Metamorphic evolution of the northwestern Ogcheon metamorphic belt,South Korea[J].Lithos,43(1):31~51.
Mitchell R J and Harley S L.2017.Zr-in-rutile resetting in aluminosilicate bearing ultra-high temperature granulites:Refining the record of cooling and hydration in the Napier Complex,Antarctica[J].Lithos,272~273:128~146.
Moazzen M.2004.Chlorite-chloritoid-garnet equilibria and geothermometry in the Sanandaj-Sirjan metamorphic belt,Southern Iran[J].Iranian Journal of Science and Technolagy,28(A1):65~78.
Nachlas W O,Whitney D L,Teyssier C,et al.2014.Titanium concentration in quartz as a record of multiple deformation mechanisms in an extensional shear zone[J].Geochemistry Geophysics Geosystems,15(4):1 374~1 397.
O'Brien P J and Tzler J R.2003.High-pressure granulites:formation,recovery of peak conditions and implications for tectonics[J].Journal of Metamorphic Geology,21(1):3~20.
zdamar S F,Roden M,Esenli F,et al.2012.Geochemical features and K-Ar age data from metadetrital rocks and high-K metasomatized metarhyolites in the Afyon-BolkardaZone(Ilgin-Konya),SW Turkey[J].Neues Jahrbuch für Mineralogie-Abhandlungen,189(2):155~176.
Pape J,Mezger K and Robyr M.2016.A systematic evaluation of the Zrin-rutile thermometer in ultra-high temperature(UHT)rocks[J].Contributions to Mineralogy and Petrology,171(5):1~20.
Powell R and Holland T J B.2008.On thermobarometry[J].Journal of Metamorphic Geology,26(2):155~179.
Ren Y F,Chen D L,Hauzenberger C,et al.2016.Petrology and geochronology of ultrahigh-pressure granitic gneiss from South Dulan,North Qaidam belt,NW China[J].International Geology Review,58(2):171~195.
Saki A,Moazzen M and Oberhnsli R.2012.Mineral chemistry and thermobarometry of the staurolite-chloritoid schists from Poshtuk,NWIran[J].Geological Magazine,149(6):1 077~1 088.
engün F.2017.Zr-in-rutile thermometry of eclogites from the Karakaya Complex in NW Turkey:Implications for rutile growth during subduction zone metamorphism[J].Chemie der Erde-Geochemistry,77(1):95~104.
Shatsky V S,Skuzovatov S Y,Ragozin A L,et al.2015.Mobility of elements in a continental subduction zone:Evidence from the UHP metamorphic complex of the Kokchetav massif[J].Russian Geology&Geophysics,56(7):1 016~1 034.
Shen Qihan.2009.The recommendation of a systematic list of mineral abbreviations[J].Acta Petrologica et Mineralogica,28(5):495~500(in Chinese with English abstract).
Song S G,Zhang L F,Niu Y L,et al.2007.Eclogite and carpholitebearing metasedimentary rocks in the North Qilian suture zone,NWChina:Implications for Early Palaeozoic cold oceanic subduction and water transport into mantle[J].Journal of Metamorphic Geology,25(5):547~563.
Spear F S,Wark D A,Cheney J T,et al.2006.Zr-in-rutile thermometry in blueschists from Sifnos,Greece[J].Contributions to Mineralogy and Petrology,152(3):375~385.
Stepanov A S,Daniela R,Joerg H,et al.2016.Contrasting P-T paths within the Barchi-Kol UHP terrain(Kokchetav Complex):Implications for subduction and exhumation of continental crust[J].American Mineralogist,101(4):788~807.
Tenczer V and Stüwe K.2003.The metamorphic field gradient in the eclogite type locality,Koralpe region,Eastern Alps[J].Journal of Metamorphic Geology,21(4):377~393.
Thomas J B,Watson E B,Spear F S,et al.2010.Titani Q under pressure:The effect of pressure and temperature on the solubility of Ti in quartz[J].Contributions to Mineralogy and Petrology,160(5):743~759.
Thomas J B,Watson E B,Spear F S,et al.2015.Titani Q recrystallized:Experimental confirmation of the original Ti-in-quartz calibrations[J].Contributions to Mineralogy and Petrology,169(3):1~16.
Tomkins H S,Powell R and Ellis D J.2007.The pressure dependence of the zirconium-in-rutile thermometer[J].Journal of Metamorphic Geology,25(6):703~713.
Ukar E and Cloos M.2016.Graphite-schist blocks in the Franciscan Mélange,San Simeon,California:Evidence of high-P metamorphism[J].Journal of Metamorphic Geology,34(3):191~208.
Vidal O,GofféB,Bousquet R,et al.1999.Calibration and testing of an empirical chloritoid-chlorite Mg-Fe exchange thermometer and thermodynamic data for daphnite[J].Journal of Metamorphic Geology,17(1):25~39.
Wark D A and Watson E B.2006.Titani Q:a titanium-in-quartz geothermometer[J].Contributions to Mineralogy and Petrology,152(6):743~754.
Watson E B and Harrison T M.2005.Zircon thermometer reveals minimum melting conditions on earliest Earth[J].Science,308(5 723):841~844.
Watson E B,Wark D A and Thomas J B,2006.Crystallization thermometers for zircon and rutile[J].Contributions to Mineralogy and Petrology,151(4):413~433.
Wei Chunjing.2011.Approaches and advancement of the study of metamorphic p-T-t paths[J].Earth Science Frontiers,18(2):1~16(in Chinese with English abstract).
Wei C J and Powell R.2003.Phase relations in high-pressure metapelites in the system KFMASH(K2O-Fe O-Mg O-Al2O3-Si O2-H2O)with application to natural rocks[J].Contributions to Mineralogy and Petrology,145(3):301~315.
Wei C J,Qian J H and Tian Z L.2013.Metamorphic evolution of medium-temperature ultra-high pressure(MT-UHP)eclogites from the South Dabie orogen,Central China:an insight from phase equilibria modelling[J].Journal of Metamorphic Geology,31(7):755~774.
Wei C J and Song S G.2010.Chloritoid-glaucophane schist in the North Qilian orogen,NW China:Phase equilibria and P-T path from garnet zonation[J].Journal of Metamorphic Geology,26(3):301~316.
Wei Chunjing,Su Xiangli,Lou Yuxing,et al.2009.A new interpretation of the conventional thermobnbarometry in eclogites:Evidence from the calculated PT pseudosections[J].Acta Petrologica Sinica.25(9):2 078~2 088(in Chinese with English abstract).
Wei C J,Yang Y,Su X L,et al.2009.Metamorphic evolution of lowTeclogite from the North Qilian orogen,NW China:Evidence from petrology and calculated phase equilibria in the system NCKFMASHO[J].Journal of Metamorphic Geology,27(1):55~70.
Whitney D L and Evans B W.2010.Abbreviations for names of rockforming minerals[J].American Mineralogist,95(1):185~187.
Wu Jialin,Zhai Mingguo,Zhang Hong,et al.2015.A brief review of the advance of pseudosection thermobarometry[J].Acta Petrologica Sinica,31(6):1 711~1 721(in Chinese with English abstract).
Wu Yuanbao,Chen Daogong,Xia Qunke,et al.2002.In-situ trace element analyses of zircons from Dabieshan Huangzhen eclogite:Trace element characteristics of eclogite-facies metamorphic zircon[J].Chinese Science Bulletin(in English),47(16):1 398~1 401.
You Zhendong.2007.Ultrahigh presure metamorphism:A new hot spot in earth science[J].Chinese Journal of Nature,29(5):255~264,311~312(in Chinese with English abstract).
YüXiaoning,Song Shuguang,Wei Chunjing,et al.2009.Mg-carpholite metapelite and its implications for ancient oceanic subduction in the North Qilian suture zone,NW China[J].Acta Scientiarum Naturalium Universitatis Pekinensis.45(3):472~480(in Chinese with English abstract).
Zack T and Luvizottow G L.2006.Application of rutile thermometry to eclogites[J].Mineralogy and Petrology,88(1):69~85.
Zack T,Moraes R and Kronz A.2004.Temperature dependence of Zr in rutile:empirical calibration of a rutile thermometer[J].Contributions to Mineralogy and Petrology,148(4):471~488.
Zhang Hongfei and Gao Shan.2012.Geochemistry[M].Beijing:Geological Publishing House(in Chinese).
Zhang L F,Du J X,LüZ,et al.2013.A huge oceanic-type UHP metamorphic belt in southwestern Tianshan,China:Peak metamorphic age and p-T path[J].Chinese Science Bulletin,58(35):4 378~4 383.
Zheng Yongfei.1999.Oxygen isotope fractionation in carbonate and sulfate minerals[J].Geochemical Journal,33(2):109~126.
Zheng Yongfei and Chen Jiangfeng.2000.Stable Isotope Geochemistry[M].Beijing:Science Press(in Chinese).
Zheng Yongfei,Gao Xiaoying,Chen Renxu,et al.2011.Zr-in-rutile thermometry of eclogite in the Dabie orogen:Constraints on rutile growth during continental subduction-zone metamorphism[J].Journal of Asian Earth Sciences,40(2):427~451.
Zheng Yongfei and Simon K.1991.Oxygen isotope fractionation in hematite and magnetite:A theoretical calculation and application to geothermometry of metamorphic iron-formations[J].European Journal of Mineralogy,3(5):877~886.
Zheng Yongfei and Zhao Zifu.2011.Element and isotope equilibration between minerals:Thermodynamic and kinetic controls of geothermometry and isochron dating[J].Acta Petrologica Sinica,27(2):345~364(in chinese with English abstract).
陈振宇,余金杰,李晓峰,等.2007.金红石Zr温度计在苏鲁-大别榴辉岩研究中的应用:问题讨论[J].地质学报,81(10):1 369~1 377.
陈燕,魏春景,张景森,等.2005.大别山南部高压-超高压变质地体中云母片岩和片麻岩的相平衡研究[J].岩石学报,21(6):151~162.
刘晓春,娄玉行,董树文.2005.桐柏山地区低温榴辉岩变质作用的p-T轨迹[J].岩石学报,21(4):1 081~1 093.
吕增,张立飞,曲军锋,等.2007.新疆西南天山哈布腾苏一带榴辉岩的岩石学特征及变质作用p-T轨迹[J].岩石学报,23(7):1 617~1 626.
沈其韩.2009.推荐一个系统的矿物缩写表[J].岩石矿物学杂志,28(5):495~500.
魏春景.2011.变质作用p-T-t轨迹的研究方法与进展[J].地学前缘,18(2):1~16.
魏春景,苏香丽,娄玉行,等.2009.榴辉岩中传统地质温压计新解:来自PT视剖面图的证据[J].岩石学报,25(9):2 078~2 088.
吴佳林,翟明国,张红,等.2015.视剖面图温压计研究进展评述[J].岩石学报,31(6):1 711~1 721.
吴元保,陈道公,夏群科,等.2002.大别山黄镇榴辉岩锆石的微区微量元素分析:榴辉岩相变质锆石的微量元素特征[J].科学通报,47(11):859~863.
杨蔚,林杨挺,郝佳龙,等.2013.亚微米尺度锆石微量元素分布:对锆石Ti温度计的制约[A].中国矿物岩石地球化学学会学术年会[C].
游振东.2007.超高压变质作用:地球科学的新热点[J].自然杂志,29(5):255~264,311~312.
于孝宁,宋述光,魏春景,等.2009.北祁连山含镁纤柱石高压泥质岩及其对古大洋俯冲的意义[J].北京大学学报(自然科学版),45(3):472~480.
张宏飞,高山.2012.地球化学[M].北京:地质出版社.
张立飞,杜瑾雪,吕增,等.2013.新疆西南天山超高压变质带的空间分布、峰期变质时代和p-T轨迹特征[J].科学通报,58(22):2 107~2 112.
郑永飞,陈江峰.2000.稳定同位素地球化学[M].北京:科学出版社.
郑永飞,赵子福.2011.矿物之间的元素和同位素平衡:地质测温和等时线定年的热力学和动力学控制[J].岩石学报,27(2):345~364.