Received date: 1999-11-23
Revised date: 2000-03-17
Online published: 2000-08-01
Geological timing methods established(isotopic method, paleontologic method,paleomagnetic method)set the“absolute age”or relative era of certain time in the geological process.But there have been no direct methods to measure the time limits of geological processes whether abroad or domestically so far. The tectonic chemical timing method we discussed, here is a new method which fixed the approxi-mate quantification of time limits in the tectonic geological processes.
LIU De-liang, CAO Gao-she, YANG Xiao-yong,FANG Guo-qing . EXPLORATION OF THE TIMING METHODS OF TECTONIC PROCESS[J]. Advances in Earth Science, 2000 , 15(4) : 467 -469 . DOI: 10.11867/j.issn.1001-8166.2000.04.0467
[1]刘德良,苏永军.宿松变质磷矿成矿时限的显微构造和地球化学分析[J].科学通报,1995,40(15):1 406～1 408.
[2]Liu De Liang,Su Yong Jun. Microstructural and geochemical analysis on the mineralized time series [J].Chinese Science Bulletin,1996,41(13):1 112～1 115.
[3]Twiss R J. Theory and applicability of a recrystalized grain size paleopiezometer[J].Pure Appl Geophys Res Lett,1977,5:337～340.
[4]Twiss R J. Variable entity piezometric equations for dislocation density and subgrain diameter and their relevance to olivine and quartz: in mineral and rock deformation, laboratory studies[J]. In: Hobbs B E,et al. eds. Geophysical Monography,1986, 36:247～261.
[5]Mercier R J. Stress in the lithophere: inferences from stead state flow of rocks[J].Pure Appl Geophys,1977,115:199～226.
[6]Parrish D K,Ross J V. Experimental deformation of anhydrite and early strain history of salt domes[abstr][J].Am Geophys Union Trans,1976,57:332.
[7]Grant J A. The isocon diagram a simple solution to Gresen' s Equation for metasomatic alteration[J].Eco Geol,1986,81:1976～1 982.
[8]Van der wal D,Chopra P,Drury M F,et al. Relationships between dynamically recrystallized grain size and deformation conditions in experimentally deformed olivine rocks[J].Geo-physics Research Letters,1993,20:1 479～1 482.
[9]Schmid S M,Paterson M S, Bolard J N.High temperature flow and dynamic recrystallization in carrara marble [J].Tectonophysics,1980,65:245～280.
[10]Guillope M,Poirier J P. Dynamic recrystallization during creep of single-crystalline halite:an experimental study[J].Journal of Geophysics Research,1979,84:5 557～5 567.
[11]Post A, Tullis J. A recrystallized grain size piezometer for experimentally deformed feldspar aggregates[J]. Tectono-physics, 1999,303:159～173.
[12]Hirth G,Tullis J. Dislocation creep regimes in quartz aggregates[J]. Journal of Structural Geology,1992,14:149～159.
[13]Shelton G.Tullis J. Experimental flow laws for crustal rocks[J].EOS,1981,62:396.
[14]Kronenberg A K,Tullis J. Flow strengths of quartz aggregates: grain size and pressure effects due to hydrolytic weakening[J]. Journal of Geophysics Research,1984,89:4 281～4 297.
[15]Jaoul O,Tullis J,Kronenberg A. The effect of varying water content on the creep behavior of Heaviterr Quartzite [J].Journal of Geophysics Research,1984,89:4 298～4 312.
[16]Koch P S,Christie J M,Ore A. Effect of water on the rheology of experimentally deformed quartzite[J],Journal of Geophysics Letters,1989,94: 13 957～13 996.
[17]Gleason G C, Tullis J. A flow law for dislocation creep of quartz aggregates determined with the molten salt cell[J].Tectonophysics, 1995,247:1～23.
/
| 〈 |
|
〉 |
