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- W2359286731 abstract "The effective heating time for apatite fission track ranges from 200 to 300 Ma in the Ordos Basin. The annealing zone in the western margin of the basin is shallow and wide,having its paleotemperature gradient (1. 5-2. 1 ℃ /100m) less than that (1. 9-2. 5 ℃ /100m) of the present time, while the annealing zone in main part of the basin is relatively deep and narrow, having its paleotemperature gradient (3. 8-4. 7℃ /100m) much bigger than that (2. 0-3. 1℃/100m) of the present time. The results of the apatite fission track analysis shows that there are three times tectonothermal events (215 Ma. 135 Ma and 72 Ma) in Ordos basin since late Paleozoic." @default.
- W2359286731 created "2016-06-24" @default.
- W2359286731 creator A5072275895 @default.
- W2359286731 date "1996-01-01" @default.
- W2359286731 modified "2023-09-25" @default.
- W2359286731 title "PALEOTEMPERATURE BY APATITE FISSION TRACK IN THE ORDOS BASIN, NW CHINA" @default.
- W2359286731 hasPublicationYear "1996" @default.
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