流体地球科学与地球系统科学
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摘要
近年来,地球系统科学逐渐成为地球科学的新趋势,但固体地球科学尚难于融入其中。其根本原因在于地球系统科学属于系统科学或复杂科学的组成部分,而固体地球科学其本质上属于理想科学的范畴,以研究线性地球过程为主,或者以理想科学的手法研究非线性地球过程。流体地球科学不仅研究地球的流体系统,也研究流体系统与固体系统的强和弱相互作用,是固体地球科学融入地球系统科学的唯一途径。
In recent years,Earth System Science(ESS)gradually becomes the new trend of the Earth Science.However,Solid Earth Science(SES)has hardly merged with it.This is because ESS is the application of system-or complex-science to the Earth Science,while SES is essentially a category of pure Earth Science,in which linear Earth processes are mainly concerned,or non-linear Earth processes are researched using pure Earth science approaches.Fluid Earth Science(FES),on the other hand,not only encompasses studies of the fluid system of the Earth,but also the strong and weak interactions between fluid and solid systems.Consequently,only FES can mediate the integration of SES into ESS.
In recent years,Earth System Science(ESS)gradually becomes the new trend of the Earth Science.However,Solid Earth Science(SES)has hardly merged with it.This is because ESS is the application of system-or complex-science to the Earth Science,while SES is essentially a category of pure Earth Science,in which linear Earth processes are mainly concerned,or non-linear Earth processes are researched using pure Earth science approaches.Fluid Earth Science(FES),on the other hand,not only encompasses studies of the fluid system of the Earth,but also the strong and weak interactions between fluid and solid systems.Consequently,only FES can mediate the integration of SES into ESS.
引文
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[12]罗照华,卢欣祥,许俊玉,等.成矿侵入体的岩石学标志[J].岩石学报,2010,26(8):2247-2254.
[13]MARSH B D.On some fundamentals of igneous petrology[J].Contributions to Mineralogy and Petrology,2013,166(3):665-690.
[14]BARER D R.Granitic melt viscosity and dike formation[J].Journal of Structural Geology,1998,20(9):1395-1404.
[15]杜建国,仵柯田,孙凤霞.地震成因综述[J].地学前缘,2018,25(4):255-267.
[16]杜乐天.地球的五个气圈与氢、烃资源:兼论气体地球动力学[J].铀矿地质,1993,9(5):257-265.
[17]杜乐天.地球排气作用:建立整体地球科学的一条统纲[J].地学前缘,2000,7(2):381-390.
[18]PLANK T,KELLEY K A,ZIMMER M M,et al.Why do mafic arc magmas contain~4wt%water on average?[J].Earth and Planetary Science Letters,2013,364:168-179.
[19]WEINBERG R F,HASALOVP.Water-fluxed melting of the continental crust:a review[J].Lithos,2015,212/213/214/215(1):158-188.
[20]BUREAU H,KEPPLER H.Complete miscibility between silicate melts and hydrous fluids in the upper mantle:experimental evidence and geochemical implications[J].Earth and Planetary Science Letters,1999,165(2):187-196.
[2]毕思文.地球系统科学综述[J].地球物理学进展,2004,19(3):504-514.
[3]於崇文.地质系统的复杂性(上、下册)[M].北京:地质出版社,2003:1135.
[4]罗照华,卢欣祥,陈必河,等.透岩浆流体成矿作用导论[M].北京:地质出版社,2009:1-177.
[5]罗照华,刘翠,苏尚国.理解岩浆系统的物理过程[J].岩石学报,2014,30(11):3113-3119.
[6]CARMICHAEL I S E,TUNER F J,VERHOOGEN J.Igneous petrology[M].New York:McGraw-Hill,1974:1-739.
[7]PARMIGIANI A,HUBER C,BACHMANN O.Mush microphysics and the reactivation of crystal-rich magma reservoirs[J].Journal of Geophysical Research:Solid Earth,2014,119(8):6308-6322.
[8]刘璐璐,苏尚国,侯建光,等.河北武安坦岭多斑斜长斑岩的成因:冻结岩浆房活化机制[J].岩石学报,2017,33(1):204-220.
[9]罗照华,郭晶,黑慧欣,等.东昆仑造山带家琪式斑岩型CuMo矿床中花岗闪长岩的斜长石晶体群及其成矿意义[J].矿物岩石地球化学通报,2018,37(2):214-228.
[10]COUCH S,SPARKS R S J,CARROLL M R.Mineral disequilibrium in lavas explained by convective self-mixing in open magma chambers[J].Nature,2001,411:1037-1039.
[11]BACHMANN O,BERGANTZ G W.Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies[J].Journal of Volcanology and Geothermal Research,2006,149(1):85-102.
[12]罗照华,卢欣祥,许俊玉,等.成矿侵入体的岩石学标志[J].岩石学报,2010,26(8):2247-2254.
[13]MARSH B D.On some fundamentals of igneous petrology[J].Contributions to Mineralogy and Petrology,2013,166(3):665-690.
[14]BARER D R.Granitic melt viscosity and dike formation[J].Journal of Structural Geology,1998,20(9):1395-1404.
[15]杜建国,仵柯田,孙凤霞.地震成因综述[J].地学前缘,2018,25(4):255-267.
[16]杜乐天.地球的五个气圈与氢、烃资源:兼论气体地球动力学[J].铀矿地质,1993,9(5):257-265.
[17]杜乐天.地球排气作用:建立整体地球科学的一条统纲[J].地学前缘,2000,7(2):381-390.
[18]PLANK T,KELLEY K A,ZIMMER M M,et al.Why do mafic arc magmas contain~4wt%water on average?[J].Earth and Planetary Science Letters,2013,364:168-179.
[19]WEINBERG R F,HASALOVP.Water-fluxed melting of the continental crust:a review[J].Lithos,2015,212/213/214/215(1):158-188.
[20]BUREAU H,KEPPLER H.Complete miscibility between silicate melts and hydrous fluids in the upper mantle:experimental evidence and geochemical implications[J].Earth and Planetary Science Letters,1999,165(2):187-196.