基于碎屑磷灰石裂变径迹热史判别碎屑岩形成时代的方法
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摘要
查明碎屑沉积岩的形成时代是正确进行地层对比、合理恢复盆地原貌、准确认识区域构造演化和科学进行油气资源评价的前提.依据"沉积物埋藏深度增加,其温度相应增加"的原理,可将碎屑磷灰石热史模拟中的初始升温阶段所对应的时间,定义为碎屑岩的形成时代;利用碎屑岩内磷灰石矿物的裂变径迹热史模拟成果,可确定赋存磷灰石矿物的沉积岩(物)的热演化史;根据模拟的沉积岩(物)热史中初始埋藏增温时间便可确定该碎屑沉积岩(物)沉积的时代.前人大量碎屑磷灰石裂变径迹热史模拟实例和六盘山砂岩磷灰石裂变径迹热史模拟成果证明,磷灰石裂变径迹热史确定碎屑岩的形成时代是可行的,利用"经历埋藏温度小于封闭温度的未退火或部分退火"碎屑岩样品的磷灰石裂变径迹热史来确定该碎屑岩形成时代是可信的.
The dating of formation age of clastic rock is the premise of the division and correlation of sedimentary strata, reasonable reconstruction of prototype basin, better understanding of the regional tectonic evolutions and scientific evaluation of regional resources. According to the principle of "the temperature of sediments or sedimentary rocks increases with increasing burial depth", the formation age of clastic rock can be determined by the initial burial warming time of thermal history which can be reconstructed by means of apatite fission track(AFT) thermal history simulation.Previous applications of AFT thermal history simulation and the example of sandstone sample of Liupanshan indicate that it is feasible to date the formation age of clastic rock by the simulated thermal evolution history, using clastic samples that experienced burial temperatures of less than the closure temperature in the thermal history simulation of fission track.
The dating of formation age of clastic rock is the premise of the division and correlation of sedimentary strata, reasonable reconstruction of prototype basin, better understanding of the regional tectonic evolutions and scientific evaluation of regional resources. According to the principle of "the temperature of sediments or sedimentary rocks increases with increasing burial depth", the formation age of clastic rock can be determined by the initial burial warming time of thermal history which can be reconstructed by means of apatite fission track(AFT) thermal history simulation.Previous applications of AFT thermal history simulation and the example of sandstone sample of Liupanshan indicate that it is feasible to date the formation age of clastic rock by the simulated thermal evolution history, using clastic samples that experienced burial temperatures of less than the closure temperature in the thermal history simulation of fission track.
引文
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Deng,J.,Yang,L.Q.,Sun,Z.S.,et al.,2000.Ore-Forming Dynamics of Tectonic Regime Transformation and Multi-Layer Fluid Circulation.Earth Science,25(4):397-403(in Chinese with English abstract).
Dickinson,W.R.,Gehrels,G.E.,2009.Use of U-Pb Ages of Detrital Zircons to Infer Maximum Depositional Ages of Strata:A Test against a Colorado Plateau Mesozoic Database.Earth and Planetary Science Letters,288(1-2):115-125.https://doi.org/10.1016/j.epsl.2009.09.013
Duddy,I.R.,Green,P.F.,Laslett,G.M.,1988.Thermal Annealing of Fission Tracks in Apatite 3. Variable Temperature Behaviour.Chemical Geology:Isotope Geoscience Section, 73(1):25-38.https://doi.org/10.1016/0168-9622(8 8)90019-x
Fernandes,P.,Cogne,N.,Chew,D.M.,et al.,2015.The Thermal History of the Karoo Moatize-Minjova Basin, Tete Province, Mozambique:An Integrated Vitrinite Reflectance and Apatite Fission Track Thermochronology Study. Journal of African Earth Sciences, 112:55-72. https://doi.org/10.1016/j.jafrearsci.2015.09.009
Gleadow,A J.W.,Duddy,I.R.,Lovering,J.F.,1983.Fission Track Analysis:A New Tool for the Evaluation of Thermal Histories and Hydrocarbon Potential. The APPEA Journal,23(1):93-102.https://doi.org/10.1071/aj82009
Gleadow,A.J.W.,Duddy,I.R.,Green,P.F.,et al. 1986. Fission Track Lengths in the Apatite Annealing Zone and the Interpretation of Mixed Ages. Earth and Planetary Science Letters, 78(2-3):245-254.https://doi.org/10.1016/0012-821x(86)90065-8
Green,P.F.,Duddy,I.R.,Gleadow,A.J.W., 1986. Thermal Annealing of Fission Tracks in Apatite 1. A Qualitative Description. Chemical Geology:Isotope Geoscience Section, 59:237-253. https://doi.org/10.1016/0009-2 541(86)90048-3
Guo,C.L.,Wu,F.Y.,2003.High Precision Dating of Deposition of Clastic Sedimentary Rocks—U-Pb SHRIMP Dating on Authigenic Xenotime.Earth Science Frontiers,10(2):327-334(in Chinese with English abstract).
Hu,R.G.,Bai,X.J.,Wijbrans,J.,et al.,2018.Occurrence of Excess 40Ar in Amphibole:Implications of 40Ar/39Ar Dating by Laser Stepwise Heating and in vacuo Crushing.Journal of Earth Science,29(2):416-426.
Ketcham,R.A.,2005.Forward and Inverse Modeling of LowTemperature Thermochronometry Data. Reviews in Mineralogy and Geochemistry, 58(1):275-314. https://doi.org/10.2138/rmg.2005.58.11
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