山东铁铜沟橄榄岩的水含量：华北克拉通早白垩世富水岩石圈的分布

夏群科; 程徽; 刘佳

doi:10.3799/dqkx.2017.075

Volume 42 Issue 6

Jun. 2017

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2017 > 42(6): 853-861

Xia Qunke, Cheng Hui, Liu Jia, 2017. The Distribution of the Early Cretaceous Hydrous Lithospheric Mantle in the North China Craton: Constraints from Water Content in Peridotites of Tietonggou. Earth Science, 42(6): 853-861. doi: 10.3799/dqkx.2017.075

Citation:

Xia Qunke, Cheng Hui, Liu Jia, 2017. The Distribution of the Early Cretaceous Hydrous Lithospheric Mantle in the North China Craton: Constraints from Water Content in Peridotites of Tietonggou. Earth Science, 42(6): 853-861. doi: 10.3799/dqkx.2017.075

Citation:

Xia Qunke, Cheng Hui, Liu Jia, 2017. The Distribution of the Early Cretaceous Hydrous Lithospheric Mantle in the North China Craton: Constraints from Water Content in Peridotites of Tietonggou. Earth Science, 42(6): 853-861. doi: 10.3799/dqkx.2017.075

PDF( 1859 KB)

The Distribution of the Early Cretaceous Hydrous Lithospheric Mantle in the North China Craton: Constraints from Water Content in Peridotites of Tietonggou

doi: 10.3799/dqkx.2017.075

Xia Qunke^{1,2
,},
Cheng Hui¹,
Liu Jia^1,2

1.
School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
2.
School of Earth Sciences, Zhejiang University, Hangzhou 310027, China

Received Date: 2017-05-10
Publish Date: 2017-06-15

Abstract

Abstract

Previous studies show that the Early Cretaceous lithospheric mantle beneath Feixian (Shandong Province) in the eastern part of the North China Craton (NCC) was highly hydrous ( > 1 000×10^-6, H₂O wt.), in which the H₂O content of olivine was > 180×10^-6. Meanwhile the Early Cretaceous lithospheric mantle beneath Fushan (Shanxi Province) in the western part of the NCC was relatively dry, in which the H₂O content of olivine was ~10×10^-6. This contrast demonstrates that the hydration of the Early Cretaceous lithospheric mantle of eastern NCC was probably due to the westward subduction of the Pacific plate, and this high water content had significantly reduced the viscosity of the lithospheric mantle and provided a prerequisite for the destruction of the NCC. To explore the distribution of hydrous lithospheric mantle in the NCC, we measured the H₂O content of the peridotite xenoliths hosted by the Early Cretaceous high-magnesium diorites of Tietonggou (Shandong Province) that is located between Feixian and Fushan.The H₂O content of olivine in the Tietonggou peridotites is (6-24)×10^-6 (average (15±7)×10^-6) and comparable with that of the Fushan olivine, suggesting that the Early Cretaceous hydrous lithospheric mantle caused by the westward subduction of the Pacific plate was likely limited to the most eastern part of the NCC.
- water content,
- peridotite,
- Early Cretaceous,
- Tietonggou,
- destruction of NCC,
- petrology,
- geochemistry

FullText(HTML)

References(37)

References

Bell, D.R., Ihinger, P.D., Rossman, G.R., 1995.Quantitative and Analysis of Trace OH in Garnet and Pyroxenes.Am. Mineral., 80(5-6):465-474. doi: 10.2138/am-1995-5-607

Bell, D.R., Rossman, G.R., 1992.Water in Earth's Mantle:The Role of Nominally Anhydrous Minerals.Science, 255(5050):1391-1397. doi: 10.1126/science.255.5050.1391

Bell, D.R., Rossman, G.R., Maldener, J., et al., 2003.Hydroxide in Olivine:A Quantitative Determination of the Absolute Amount and Calibration of the IR Spectrum.Journal of Geophysical Research, 108(B2):998-1003, doi: 10.1029/2001JB000679

Berry, A.J., Hermann, J., O'Neill, H.S.C., et al., 2005.Fingerprinting the Water Site in Mantle Olivine.Geology, 33(11):869-872.doi: 10.1130/G21759.1

Chen, L.H., Zhou, X.H., 2005.Subduction-Related Metasomatism in the Thinning Lithosphere:Evidence from a Composite Dunite-Orthopyroxenite Xenolith Entrained in Mesozoic Laiwu High-Mg Diorite, North China Craton.Geochem. Geophys. Geosyst., 6(6):453-468.doi: 10.1029/2005GC000938

Denis, C.M.M., Alard, O., Demouchy, S., 2015.Water Content and Hydrogen Behavior during Metasomatism in the Uppermost Mantle beneath Ray Pic Volcano (Massif Central, France).Lithos, 237:256-274. https://www.researchgate.net/profile/Carole_Denis/publication/282333223_Water_content_and_hydrogen_behaviour_during_metasomatism_in_the_uppermost_mantle_beneath_Ray_Pic_volcano_Massif_Central_France/links/560cef7308aed543358d54ed/Water-content-and-hydrogen-behaviour-during-metasomatism-in-the-uppermost-mantle-beneath-Ray-Pic-volcano-Massif-Central-France.pdf

Dixon, J.E., Dixon, T.H., Bell, D.R., 2004.Lateral Variation in Upper Mantle Viscosity:Role of Water.Earth Planet. Sci. Lett., 222(2):451-467. doi: 10.1016/j.epsl.2004.03.022

Doucet, L.S., Peslier, A.H., Ionov, D., 2014.High Water Contents in the Siberian Cratonic Mantle Linked to Metasomatism:An FTIR Study of Udachnaya Peridotite Xenoliths.Geochim. Cosmochim. Acta, 137:159-187. doi: 10.1016/j.gca.2014.04.011

Downes, H., 2001.Formation and Modification of the Shallow Sub-Continental Lithospheric Mantle:A Review of Geochemical Evidence from Ultramafic Xenolith Suites and Tectonically Emplaced Ultramafic Massifs of Western and Central Europe.J. Petrol., 42(1):233-250. doi: 10.1093/petrology/42.1.233

Gose, J., Schmädicke, E., Markowitz, M., et al., 2010.OH Point Defects in Olivine from Pakistan.Mineral.Petrol., 99(1):105-111. http://www.academia.edu/17782484/OH_point_defects_in_olivine_from_Pakistan

Grant, K., Ingrin, J., Lorand, J.P., et al., 2007.Water Partitioning between Mantle Minerals from Peridotite Xenoliths.Contrib. Mineral. Petrol., 154(1):15-34. doi: 10.1007/s00410-006-0177-1

Hao, Y.T., Xia, Q.K., Li, Q.W., et al., 2014.Partial Melting Control of Water Contents in the Cenozoic Lithospheric Mantle of the Cathaysia Block of South China.Chem.Geol., 380:7-19. doi: 10.1016/j.chemgeo.2014.04.017

Hao, Y.T., Xia, Q.K., Tian, Z.Z., et al., 2016.Mantle Metasomatism did not Modify the Water Content of the Peridotite Xenoliths from the Tianchang Basalts of Eastern China.Lithos, 260:315-327. doi: 10.1016/j.lithos.2016.06.003

Hirschmann, M.M., 2005.Water, Melting, and the Deep Earth H₂O Cycle.Annu. Earth Planet. Sci., 2334(34):629-653.

Kovács, I., Green, D.H., Rosenthal, A., et al., 2012.An Experimental Study of Water in Nominally Anhydrous Minerals in the Upper Mantle near the Water-Saturated Solidus.J. Petrol., 53(10):2067-2093. doi: 10.1093/petrology/egs044

Kovács, I., Hermann, J., O'Neill, H.S.C., et al., 2008.Quantitative Absorbance Spectroscopy with Unpolarized Light:Part Ⅱ.Experimental Evaluation and Development of a Protocol for Quantitative Analysis of Mineral IR Spectra.Am. Mineral., 93(5-6):765-778.doi: 10.2138/am.2008.2657

Lee, C.T., Luffi, P., Chin, E.J., 2011.Building and Destroying Continental Mantle.Annual Review of Earth & Planetary Sciences, 39(39):59-90. http://www.academia.edu/14386783/Building_and_destroying_continental_mantle

Li, Z.X.A., Lee, C.T., Peslier, A.H., et al., 2008.Water Contents in Mantle Xenoliths from the Colorado Plateau and Vicinity:Implications for the Mantle Rheology and Hydration-Induced Thinning of Continental Lithosphere.J.Geophys.Res., 113(B9):B09210.doi: 1029/2007JB005540

Liu, S.C., Xia, Q, K., 2014.Water Content in the Early Cretaceous Lithospheric Mantle beneath the South-Central Taihang Mountains:Implications for the Destruction of the North China Craton.Chinese Science Bulletin, 59(13):1362-1365. doi: 10.1007/s11434-014-0203-z

Matveev, A., Portnyagin, M., Ballhaus, C., et al., 2005.FTIR Spectrum of Phenocryst Olivine as an Indicator of Silica Saturation in Magmas.J. Petrol., 46(3):603-614. https://www.researchgate.net/publication/235766932_FTIR_Spectrum_of_Phenocryst_Olivine_as_an_Indicator_of_Silica_Saturation_in_Magmas

Menzies, M.A., Xu, Y.G., Zhang, H.F., et al., 2007.Integration of Geology, Geophysics and Geochemistry:A Key to Understanding the North China Craton.Lithos, 96:1-21. doi: 10.1016/j.lithos.2006.09.008

Peslier, A.H., Woodland, A.B., Bell, D.R., et al., 2010.Olivine Water Contents in the Continental Lithosphere and the Longevity of Cratons.Nature, 467(7311):78-81. doi: 10.1038/nature09317

Peslier, A.H., Woodland, A.B., Bell, D.R., et al., 2012.Metasomatic Control of Water Contents in the Kaapvaal Cratonic Mantle.Geochim.Cosmochim.Acta, 97(97):213-246.

Proietti, A., Bystricky, M., Guignard, J., et al., 2016.Effect of Pressure on the Strength of Olivine at Room Temperature.Phys. Earth Planet Inter., 259:34-44. doi: 10.1016/j.pepi.2016.08.004

Schmädicke, E., Gose, J., Witt-Eickschen, G., et al., 2013.Olivine from Spinel Peridotite Xenoliths:Hydroxyl Incorporation and Mineral Composition.Am.Mineral., 98(10):1870-1880. doi: 10.2138/am.2013.4440

Xia, Q.K., Hao, Y.T., Li, P., et al., 2010.Low Water Content of the Cenozoic Lithospheric Mantle beneath the Eastern Part of the North China Craton.J.Geophys.Res., 115(B7):1-22.doi: 10.1029/2009JB006694

Xia, Q.K., Liu, J., Kovács, I., et al., 2017.Water in the Upper Mantle and Deep Crust of Eastern China:Concentration, Distribution and Implications.National Science Review.doi:10.1093/nsr/nwx016

Xia, Q.K., Liu, J., Liu, S.C., et al., 2013.High Water Content in Mesozoic Primitive Basalts of the North China Craton and Implications for the Destruction of Cratonic Mantle Lithosphere.Earth Planet. Sci. Lett., 361(1):85-97. http://www.academia.edu/2358045/High_watercontent_in_Mesozoic_primitive_basalts_of_the_North_China_Craton_and_implications_on_the_destruction_of_cratonic_mantle_lithosphere

Xu, W.L., Hergt, J.M., Gao, S., et al., 2008.Interaction of Adakitic Melt-Peridotite:Implications for the High-Mg^# Signature of Mesozoic Adakitic Rocks in the Eastern North China Craton.Earth Planet.Sci.Lett., 265(1-2):123-137. doi: 10.1016/j.epsl.2007.09.041

Xu, W.L., Wang, D.Y., Wang, Q.H., et al., 2003.Petrology and Geochemisty of Two Types of Mantle-Derived Xenoliths in Mesozoic Diorite from Western Shandong Province.Acta Petrologica Sinica, 19(4):623-636(in Chinese with English abstract). https://www.researchgate.net/publication/285731412_Petrology_and_geochemistry_of_two_types_of_mantle-derived_xenoliths_in_Mesozoic_diorite_from_western_Shandong_province

Xu, W.L., Yang, D.B., Gao, S., et al., 2010.Geochemistry of Peridotite Xenoliths in Early Cretaceous High-Mg^# Diorites from the Central Orogenic Block of the North China Craton:The Nature of Mesozoic Lithospheric Mantle and Constraints on Lithospheric Thinning.Chem.Geol., 270(1-4):257-273. doi: 10.1016/j.chemgeo.2009.12.006

Yamamoto, J., Ando, J., Kagi, H., et al., 2008.In Situ Strength Measurements on Natural Upper-Mantle Minerals.Phys. Chem. Minerals, 35:249-257.doi: 10.1007/s00269-008-0218-6

Yang, D.B., Xu, W.L., Gao, S., et al., 2012.Repeated Modification of Lithospheric Mantle in the Eastern North China Craton:Constraints from SHRIMP Zircon U-Pb Dating of Dunite Xenoliths in Western Shandong.Chinese Science Bulletin, 57(6):651-659. doi: 10.1007/s11434-011-4852-x

Zhang, J., Zhang, H.F., Ying, J.F., et al., 2005.Are the Peridotitic Xenoliths Entrained in Late Mesozoic Intermediate-Mafic Intrusive Complexes on the North China Craton the Direct Samples of Lithospheric Mantle? Acta Petrologica Sinica, 21(6):1559-1568(in Chinese with English abstract). https://www.researchgate.net/publication/305532219_Are_the_peridotitic_xenoliths_entrained_in_Late_Mesozoic_intermediate-mafic_intrusive_complexes_on_the_North_China_Craton_the_direct_samples_of_lithospheric_mantle

Zhu, R.X., Xu, Y.G, Zhu, G., et al., 2012.Destruction of the North China Craton.Sci. China:Earth Sci., 55(10):1565-1587. doi: 10.1007/s11430-012-4516-y

许文良, 王冬艳, 王清海, 等, 2003.鲁西中生代闪长岩中两类幔源捕掳体的岩石学和地球化学.岩石学报, 19(4):623-636. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200304003.htm

张瑾, 张宏福, 英基丰, 等, 2005.华北晚中生代中基性侵入体中橄榄岩捕掳体是岩石圈地幔直接样品?岩石学报, 21(6):1559-1568. http://cdmd.cnki.com.cn/Article/CDMD-10358-1011124978.htm

Relative Articles

Supplements(0)

Cited By

Proportional views