Micro-area Chemical Composition and Preserved P-T Evolution Trace of Phengite in Albite Gneiss from the Donghai Ultrahigh-Pressure Metamorphic Area, East China
Study of micro‐area chemical compositions indicates that phengite in albite gneiss from hole ZK2304 of the Donghai region has evident compositional zoning. SiO2 and tetrahedrally coordinated Si contents decrease, and Al2O3, AlIVand AlVIcontents increase gradually from core to rim. However, K2O, MgO...
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| Published in | Acta geologica Sinica (Beijing) Vol. 74; no. 2; pp. 183 - 189 |
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| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
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Oxford, UK
Blackwell Publishing Ltd
01.06.2000
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| Abstract | Study of micro‐area chemical compositions indicates that phengite in albite gneiss from hole ZK2304 of the Donghai region has evident compositional zoning. SiO2 and tetrahedrally coordinated Si contents decrease, and Al2O3, AlIVand AlVIcontents increase gradually from core to rim. However, K2O, MgO and FeO contents basically remain unchanged from core to rim. According to P‐T estimates obtained from geothermometers and barometers, combined with previous experimental data, the core belt (micro‐area I) of phengite was formed at T=637–672°C and P=1.55–1.73 GPa, and the transitional belt (micro‐area II) of the phengite were formed at T=594–654°C and P=1.35–1.45 GPa. Towards the rim belt (micro‐area III), the temperature decreased slightly, but the pressure decreased rapidly with T=542–630°C and P=1.12–1.19 GPa. The P‐T evolution path recorded by the compositional zoning of phengite is characterized by significant near‐isothermal decompression, revealing that the gneiss has undergone high‐pressure‐ultrahigh‐pressure metamorphism. The compositional zoning of the phengite in the albite gneiss may have formed in the geodynamic process of rapid exhumation in the Sulu ultrahigh‐pressure metamorphic belt. |
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| AbstractList | Study of micro‐area chemical compositions indicates that phengite in albite gneiss from hole ZK2304 of the Donghai region has evident compositional zoning. SiO2 and tetrahedrally coordinated Si contents decrease, and Al2O3, AlIVand AlVIcontents increase gradually from core to rim. However, K2O, MgO and FeO contents basically remain unchanged from core to rim. According to P‐T estimates obtained from geothermometers and barometers, combined with previous experimental data, the core belt (micro‐area I) of phengite was formed at T=637–672°C and P=1.55–1.73 GPa, and the transitional belt (micro‐area II) of the phengite were formed at T=594–654°C and P=1.35–1.45 GPa. Towards the rim belt (micro‐area III), the temperature decreased slightly, but the pressure decreased rapidly with T=542–630°C and P=1.12–1.19 GPa. The P‐T evolution path recorded by the compositional zoning of phengite is characterized by significant near‐isothermal decompression, revealing that the gneiss has undergone high‐pressure‐ultrahigh‐pressure metamorphism. The compositional zoning of the phengite in the albite gneiss may have formed in the geodynamic process of rapid exhumation in the Sulu ultrahigh‐pressure metamorphic belt. Abstract Study of micro‐area chemical compositions indicates that phengite in albite gneiss from hole ZK2304 of the Donghai region has evident compositional zoning. SiO 2 and tetrahedrally coordinated Si contents decrease, and Al 2 O 3 , Al IV and Al VI contents increase gradually from core to rim. However, K 2 O, MgO and FeO contents basically remain unchanged from core to rim. According to P‐T estimates obtained from geothermometers and barometers, combined with previous experimental data, the core belt (micro‐area I) of phengite was formed at T =637–672°C and P =1.55–1.73 GPa, and the transitional belt (micro‐area II) of the phengite were formed at T =594–654°C and P =1.35–1.45 GPa. Towards the rim belt (micro‐area III), the temperature decreased slightly, but the pressure decreased rapidly with T =542–630°C and P =1.12–1.19 GPa. The P‐T evolution path recorded by the compositional zoning of phengite is characterized by significant near‐isothermal decompression, revealing that the gneiss has undergone high‐pressure‐ultrahigh‐pressure metamorphism. The compositional zoning of the phengite in the albite gneiss may have formed in the geodynamic process of rapid exhumation in the Sulu ultrahigh‐pressure metamorphic belt. |
| Author | Fulai, LIU Jingsui, YANG Zeming, ZHANG Zhiqin, XU Huifen, XU |
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| Notes | ArticleID:ACGS447 istex:57703F51AB8B241E16533672E1E9E958D7F09739 ark:/67375/WNG-94STCRTZ-T liufl@cmc.com.cn Liu Fulai Born in 1963; got his doctor's degree in 1995 at the Changchun College of Geology. Now he is mainly engaged in research on metamorphic petrology. E‐mail |
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Mineral. contributor: fullname: Enami M. – ident: e_1_2_1_7_1 doi: 10.1007/BF00376087 – ident: e_1_2_1_15_1 doi: 10.1127/ejm/5/1/0141 – ident: e_1_2_1_6_1 doi: 10.1111/j.1525-1314.1997.00013.x – ident: e_1_2_1_12_1 doi: 10.1007/BF00375235 – volume: 1 start-page: 43 year: 1992 ident: e_1_2_1_20_1 article-title: Coesite‐bearing ultramafic pressure metamorphic rocks from Donghai, northern Jiangsu province, eastern China: “foreign or in situ”? publication-title: Scientica Geologica Sinica contributor: fullname: Zhao Z.Y. – volume: 45 start-page: 636 year: 1999 ident: e_1_2_1_9_1 article-title: Petrology and genetic mechanism of granitic gneiss in Donghai ultrahigh‐pressure metamorphic belt publication-title: Geological Review contributor: fullname: Fulai Liu – ident: e_1_2_1_4_1 doi: 10.1180/minmag.1990.054.377.07 – ident: e_1_2_1_8_1 doi: 10.1111/j.1755-6724.2000.tb00427.x – volume: 71 start-page: 245 issue: 3 year: 1997 ident: e_1_2_1_5_1 article-title: Evidence for the Jiangsu‐Shandong ultra‐high‐pressure metamorphic belt returns from the upper mantle to the earth surface in the Mesozoic‐Cenozoic publication-title: Acta Geological Sinica contributor: fullname: Shouxi Hu – volume: 40 start-page: 494 issue: 6 year: 1994 ident: e_1_2_1_11_1 article-title: The diversity and origin of eclogites from the Dabie‐Sulu high‐pressure metamorphic belt publication-title: Geological Review contributor: fullname: Xiaochun Liu – volume: 93 start-page: 134 issue: 2 year: 1996 ident: e_1_2_1_18_1 article-title: Petrology, metamorphic process and genesis of the Dabie‐Sulu eclogite belt, eastern‐central China publication-title: Acta Geological Sinica (Eng. ed.) doi: 10.1111/j.1755-6724.1996.mp9002003.x contributor: fullname: Zeming Zhang – ident: e_1_2_1_13_1 doi: 10.1130/0091-7613(1992)020<0411:EFITRE>2.3.CO;2 – start-page: 1 volume-title: Eclogite and Eclogite‐facies Rocks year: 1998 ident: e_1_2_1_14_1 contributor: fullname: Smith D.C. – ident: e_1_2_1_3_1 doi: 10.1016/0024-4937(82)90017-2 – ident: e_1_2_1_19_1 doi: 10.1111/j.1525-1314.1995.tb00250.x – volume: 73 start-page: 321 issue: 4 year: 1999 ident: e_1_2_1_17_1 article-title: Metamorphism of the eclogites from the ZK 703 drillhole in Donghai, south Sulu (Jiangsu‐Shandong) ultrahigh‐pressure metamorphic belt, eastern China publication-title: Acta Geological Sinica contributor: fullname: Zeming Zhang – volume: 44 start-page: 225 issue: 3 year: 1998 ident: e_1_2_1_16_1 article-title: The role of extensional tectonics in the exhumation of high‐and Ultrahigh‐pressure rocks in northern Jiangsu and southeastern Shandong publication-title: Geological Review contributor: fullname: Changhou Zhang – ident: e_1_2_1_10_1 doi: 10.1111/j.1755-6724.1999.tb00839.x |
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| Title | Micro-area Chemical Composition and Preserved P-T Evolution Trace of Phengite in Albite Gneiss from the Donghai Ultrahigh-Pressure Metamorphic Area, East China |
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