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The Tarim Basin is a representative example of the basins developed in the northwest China that are characterized by multiple stages of heating and cooling.In order to better understand its complex thermal history,apatite fssion track(AFT)thermochronology was applied to borehole samples from the Tazhong Uplift Zone(TUZ).Twelve sedimentary samples of Silurian to Triassic depositional ages were analyzed from depths coinciding with the apatite partial annealing zone(～60-120 C).The AFT ages,ranging from 132±7 Ma(from a Triassic sample)to 25±2 Ma(from a Carboniferous sample),are clearly younger than their depositional ages and demonstrate a total resetting of the AFT thermometer after deposition.The AFT ages vary among different tectonic belts and decrease from the No.Ten Faulted Zone(133-105 Ma)in the northwest,the Central Horst Zone in the middle(108-37 Ma),to the East Buried Hill Zone in the south(51-25 Ma).Given the low magnitude of post-Triassic burial heating evidenced by low vitrinite refectance values(Ro<0.7%),the total resetting of the AFT system is speculated to result from the hot fuid fow along the faults.Thermal effects along the faults are well documented by younger AFT ages and unimodal single grain age distributions in the vicinity of the faults.Permianeearly Triassic basaltic volcanism may be responsible for the early Triassic total annealing of those samples lacking connectivity with the fault.The above arguments are supported by thermal modeling results.
The Tarim Basin is a representative example of the basins developed in the northwest China that are characterized by multiple stages of heating and cooling. In order to better understand its complex thermal history, apatite fssion track (AFT) thermochronology was applied to borehole samples from the Tazhong Uplift Zone (TUZ) .Twelve sedimentary samples of Silurian to Triassic depositional ages were analyzed from depths coinciding with the apatite partial annealing zone (~ 60-120 C). AFT ages, ranging from 132 ± 7 Ma (from a Triassic sample ) to 25 ± 2 Ma (from a Carboniferous sample), are clearly younger than their depositional ages and demonstrate a total resetting of the AFT thermometer after deposition. AFT ages vary among different tectonic belts and decrease from the No.Ten Faulted Zone ( 133-105 Ma) in the northwest, the Central Horst Zone in the middle (108-37 Ma), to the East Buried Hill Zone in the south (51-25 Ma). Given the low magnitude of post-Triassic burial heating evidenced by low vitr inite refectance values (Ro <0.7%), the total resetting of the AFT system is speculated to result from the hot fuid fow along the faults.Thermal effects along the faults are well documented by younger AFT ages and unimodal single grain age distributions in the vicinity of the faults.Permianeearly Triassic basaltic volcanism may be responsible for the early Triassic total annealing of those samples lacking connectivity with the fault. Above arguments are supported by thermal modeling results.