Cretaceous-Cenozoic history of the southern Tan-Lu fault zone: apatite fission-track and structural constraints from the Dabie Shan (eastern China)
Apatite fission-track (AFT) and structural data outline the Late Cretaceous−Cenozoic history of the southern Tan-Lu fault zone (TLFZ), one of Asia's major faults, the Triassic-Jurassic Dabie orogen, Earth's largest track of ultrahigh-pressure rock exposure, and its foreland, the Yangtze fo...
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| Hauptverfasser: | , , , , , , , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
18 October 2002
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| In: |
Tectonophysics
Year: 2002, Jahrgang: 359, Heft: 3, Pages: 225-253 |
| ISSN: | 1879-3266 |
| DOI: | 10.1016/S0040-1951(02)00513-9 |
| Online-Zugang: | Verlag, Volltext: https://doi.org/10.1016/S0040-1951(02)00513-9 Verlag: http://www.sciencedirect.com/science/article/pii/S0040195102005139 
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| Verfasserangaben: | J.C. Grimmer, R. Jonckheere, E. Enkelmann, L. Ratschbacher, B.R. Hacker, A.E. Blythe, G.A. Wagner, Q. Wu, S. Liu, S. Dong |
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| 245 | 1 | 0 | |a Cretaceous-Cenozoic history of the southern Tan-Lu fault zone |b apatite fission-track and structural constraints from the Dabie Shan (eastern China) |c J.C. Grimmer, R. Jonckheere, E. Enkelmann, L. Ratschbacher, B.R. Hacker, A.E. Blythe, G.A. Wagner, Q. Wu, S. Liu, S. Dong |
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| 520 | |a Apatite fission-track (AFT) and structural data outline the Late Cretaceous−Cenozoic history of the southern Tan-Lu fault zone (TLFZ), one of Asia's major faults, the Triassic-Jurassic Dabie orogen, Earth's largest track of ultrahigh-pressure rock exposure, and its foreland, the Yangtze foreland fold-thrust belt. The fission-track analyses utilized the independent (φ-), Z- and ξ-methods for age determination, which yielded within error identical ages. Ages from Triassic-Jurassic syn-orogenic foreland sediments are younger than their depositional age and thus were reset. A group of ages records rapid cooling following shallow emplacement of granitoids of the widespread latest Jurassic−Early Cretaceous “Yanshanian” magmatism. Most ages are 90 to 55 Ma and document cooling following reheating at 110-90 Ma, the time when the basement units of the Dabie Shan were last at >200 °C. This cooling coincides with rifting marked by the Late Cretaceous−Eocene red-bed deposition in eastern China. During this period, the Dabie basements units exhumed in the footwall of the Tan-Lu fault with the Qianshan basin in the hanging wall; the associated stress field is transtensional (NW-trending principal extension direction). The youngest fission-track ages and temperature-time path modeling point to enhanced cooling in the footwall of the Tan-Lu and associated faults at 45±10 Ma. The related stress field is transtensional, with the principal extension direction changing trend from NW to W. It may be the far-field expression of the India-Asia collision superposed on the back-arc extension setting in eastern China. A regional unconformity at ∼25 Ma marks an upper bound for the inversion of the Late Cretaceous−Eocene rift structures. During the Neogene, further subsidence in the eastern China basins was accommodated by sub-horizontal NE-SW extension, and followed by the presently active NW-SE extension. The Tan-Lu fault along the eastern edge of the Dabie Shan had normal and then sinistral-transpressive motion during the Late Cretaceous−Eocene. Its motion changed during the Neogene from sinistral transtensive to normal and then to its present dextral transtensive activity. | ||
| 650 | 4 | |a Apatite fission-track thermochronology | |
| 650 | 4 | |a Dabie Shan | |
| 650 | 4 | |a Fault-slip analysis | |
| 650 | 4 | |a Late Cretaceous-Cenozoic tectonics | |
| 650 | 4 | |a Tan-Lu fault zone | |
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| 700 | 1 | |a Dong, S. |e VerfasserIn |4 aut | |
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