1887
Volume 22 Number 1
  • E-ISSN: 1365-2117

Abstract

ABSTRACT

Previously published research from the Kuqa Subbasin along northern margin of the Tarim Basin shows five tectonic‐depositional phases from Triassic to Neogene time. In order to reveal additional detailed information on the nature of provenance terrains and tectonic attributes since late Mesozoic time, five typical sandstone samples from Jurassic–Neogene strata were collected for U–Pb dating of detrital zircons. Geochronological constitution of detrital zircons of the Middle Jurassic sample is essentially unimodal and indicates major contributions from the South Tian Shan even Yili–Central Tian Shan, wherein most 370–450 Ma zircons probably resulted from tectonic accretion events between the Yili–Central Tian Shan block and South Tian Shan Ocean during Silurian and Devonian time, with sandstone provenance tectonic attributes of passive continental margin. The Lower Cretaceous sample shows a complicated provenance detrital zircon signature, with new peak ages of 290–330 Ma as well as 370(or 350)–450 Ma showing evident arc orogenic provenance tectonic attribute, probably reflecting a new provenance supply that resulted from denudation process whthin the South Tian Shan and South Tian Shan suture. There are no obvious changes within age probability spectra of detrital zircons between the Cretaceous and early Paleogene samples, which suggests that similar provenance types and basin‐range framework continued from Cretaceous to Early Paleogene time. However, unlike the Cretaceous and early Paleogene samples, an age spectra of the Miocene sample is relatively unimodal and similar to that of the Pliocene sample, with peak ages ranging between ∼392 and ∼458 Ma older than the comparable provenance ages (peak ages about 370–450 Ma) of the Middle Jurassic and Lower Cretaceous samples. Therefore, we conclude that the South Tian Shan was rapidly exhumated and the southern South Tian Shan had become the main source of clastics for the Kuqa Subbasin since the Miocene epoch.

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2009-10-26
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References

  1. Allen, M.B, Vincent, S.J. & Wheeler, P.J. (1999) Late Cenozoic tectonics of the Kepingtage thrust zone: interpretation of the Tien Shan and Tarim Basin, Northwest China. Tectonics, 18, 639–654.
    [Google Scholar]
  2. Allen, M.F. & Zhang, C. (1992) Palaeozoic collisional tectonics and magmatism of the Chinese Tien Shan, Central Asia. Tectonophysics, 220 (1–4), 89–115.
    [Google Scholar]
  3. Andersen, T. (2002) Correction of common lead in U–Pb analyses that do not report 204Pb. Chem. Geol., 192, 59–79.
    [Google Scholar]
  4. Avouac, J.P., Tapponnier, P., Bai, M.H., You, H. & Wang, G. (1993) Active thrusting and folding along the northern Tianshan and late Cenozoic rotation of the Tarim relative to Dzungaria and Kazakhstan. J. Geophys. Res., 98 (B4), 60755–60804.
    [Google Scholar]
  5. Ballard, J.R., Palin, J.M., Williams, I.S., Campbell, I.H. & Faunes, A. (2001) Two‐ages of porphyry intrusion resolved for the super‐giant Chuquicamata copper deposit of northern Chile by ELA‐ICP‐MS and SHRIMP. Geology, 29, 383–386.
    [Google Scholar]
  6. Burtman, V.S. (2000) Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir‐Tien Shan transition zone for the Cretaceous and Paleogene. Tectonophysics, 319, 69–92.
    [Google Scholar]
  7. Burtman, V.S., Skobelev, S.F. & Molnar, P. (1996) Late Cenozoic slip on the Talas‐Ferghana fault, the Tian Shan, Central Asia. Geol. Soc. Am. Bull., 108, 1004–1021.
    [Google Scholar]
  8. Carroll, A.R., Graham, S.A. & Hendrix, M.S. (1995) Late Paleozoic tectonic amalgamation of northwestern China: sedimentary record of the northern Tarim, northwestern Turpan and southern Junggar basins. Geol. Soc. Am. Bull., 107, 571–594.
    [Google Scholar]
  9. Carroll, A.R., Liang, Y., Graham, S.A., Hendrix, M.S, Ying, D. & Zhou, D. (1990) Junggar basin,northwest China, Trapped late Paleozoic ocean. Tectonophysics, 181, 1–14.
    [Google Scholar]
  10. Chen, Ch.M., Lu, H.F. & Dong, J. (1999a) Closing history of the southern Tianshan oceanic basin, western China: an oblique collisional orogeny. Tectonophysics, 302, 23–40.
    [Google Scholar]
  11. Chen, Y.B., Hu, A.Q., Zhang, G.X. & Zhang, Q.F. (1999b) Zircon U Pb geochronology of granitic gneiss at Du‐ku Highway of Southwestern Tianshan and its implications. Chin. Sci. Bull., 44 (21), 2328–2332 (in Chinese with English abstract).
    [Google Scholar]
  12. Chen, Y.B., Hu, A.Q., Zhang, G.X. & Zhang, Q.F. (1999c) Zircon U‐Pb age and Nd‐Sr isotopic composition of granitic gneiss and its geological implications from Precambrian window of western Tianshan, NW China. Geochimica, 28 (6), 515–520 (in Chinese with English abstract).
    [Google Scholar]
  13. Chen, Y.B., Hu, A.Q., Zhang, G.X. & Zhang, Q.F. (2000) Precambrian basement age and characteristics of Southwestern Tianshan: Zircon U Pb geochronology and Nd Sr isotopic compositions. Acta Petrol. Sin., 16 (1), 92–98 (in Chinese with English abstract).
    [Google Scholar]
  14. Coleman, R.G. (1989) Contiental growth of Northwest China. Tectonics, 8, 621–635.
    [Google Scholar]
  15. Dewey, J.F., Shackleton, R. & Chang, C. (1988) The Tectonic evolution of the Tibetian Plateau. Phil. Trans. R. Soc. Lond., A327, 379–413.
    [Google Scholar]
  16. Dumitru, T.A., Zhou, D., Chang, E., Graham, S.A., Hendrix, M.S., Sobel, E.R. & Carroll, A.R. (2001) Uplift, exhumation and deformation in the Chinese Tian Shan. In: Paleozoic and Mesozoic Tectonic Evolution of Central and Eastern Asia: From Continental Assembly to Intracontinental Deformation (Ed. by M.S.Hendrix & G.A.Davis , Geol. Soc. Am. Mem., 194, 71–99.
    [Google Scholar]
  17. Gao, J. & Klemd, R. (2003) Formation of HP‐LT rocks and their tectonic implications in the western Tianshan Orogen, NW China: geochemical and age constraints. Lithos, 66, 1–22.
    [Google Scholar]
  18. Gao, J., Li, M.S., Xiao, X.C., Tang, Y.H. & Guo, Q. (1998) Paleozoic tectonic evolution of the Tianshan Orogen, northwest China. Tectonophysicas, 287, 213–231.
    [Google Scholar]
  19. Gao, J., Long, L.L., Qian, Q., Su, W. & Klemd, R. (2006) South Tianshan: a Late Paleozoic or a Triassic orogen? Acta Petrol. Sin., 22 (5), 1049–1061 (in Chinese with English abstract).
    [Google Scholar]
  20. Gao, Z. (1990) Further discussion on the problem of the Precambrian stratigraphy in Tianshan area. Xinjiang Geol., 8 (1), 80–90 (in Chinese with English abstract).
    [Google Scholar]
  21. Graham, S.A, Hendrix, M.S., Wang, L.B. & Carroll, A.R. (1993) Collisional successor basins of western China: impact of tctonic inheritance on sand composition. Geol. Soc. Am. Bull., 105, 323–344.
    [Google Scholar]
  22. Guo, Z.J., Zhang, Z.C., Liu, S.W. & Li, H.M. (2003) U‐Pb geochronological evidence for the early Precambrian complex of the Tarim Craton, NW China. Acta Petrol. Sin., 19 (3), 537–542 (in Chinese with English abstract).
    [Google Scholar]
  23. Han, B.F., He, G.Q., Wu, T.R. & Li, H.M. (2004) Zircon U‐Pb dating and geochemical features of early paleozoic granites from Tianshan,Xinjiang: implications for tectonic evolution. Xinjiang Geol., 22 (1), 3–11 (in Chinese with English abstract).
    [Google Scholar]
  24. Heermance, R.V., Chen, J., Burbank, D.W. & Wang, C.S. (2007) Chronology and tectonic controls of Late Tertiary deposition in the southwestern Tian Shan foreland, NW China. Basin Res., 19 (4), 599–632.
    [Google Scholar]
  25. Hendrix, M.S. (2000) Evolution of Mesozoic sandstone compositions, southern Junggar, northern Tarim, and western Turpan basins, Northwest China: a detrital record of the ancestral Tian Shan. J. Sediment. Res., 70 (3), 520–532.
    [Google Scholar]
  26. Hendrix, M.S., Graham, S.A., Carroll, A.R., Sober, E.R., Mcknight, C.L., Shulein, B.J. & Wang, Z.X. (1992) Sedimentary record and climatic implication of recurrent deformation of the Tien Shan: evidence from Mesozoic strata of the north Tarim, south Junggar and Turpan basins. Geol. Soc. Am. Bull., 104, 53–79.
    [Google Scholar]
  27. Hu, A.Q. (2000) Crustal evolution and Phanerozoic crustal growth in northern Xinjiang: Nd isotopic evidence Part I: isotopic characterization of basement rocks. Tectonophysics, 328, 15–51.
    [Google Scholar]
  28. Hu, A.Q., Wang, Zh.G. & Tu, G.Zh. (1997) The Geologic Evolution and Diagenetic‐metallogenic Rule in the Northern Xinjiang. China Science Press, Beijing (in Chinese).
    [Google Scholar]
  29. Hu, A.Q., Zhang, G.X., Chen, Y.B. & Zhang, Q.F. (2001) A model of division of the continental Crus basement and the time scales of the major geological events in the Xinjiang‐based on studies of isotopic geochronology and geochemistry. Xinjiang Geol., 19 (1), 12–19 (in Chinese with English abstract).
    [Google Scholar]
  30. Jia, C. (1997) Structure and Oil‐Gas in Tarim Basin, China. Petroleum Industry Press, Beijing, 348–364 (in Chinese with English abstract).
    [Google Scholar]
  31. Jiang, Ch.Y., Mu, Y.M., Bai, K.Y., Zhao, X.N., Zhang, H.B. & Hei, A.Z. (1999) Chronology, petrology, geochemistry and tectonic environment of granitoids in the southern Tianshan Mountain, western China. Acta Petrol. Sin., 5 (2), 298–308 (in Chinese with English abstract).
    [Google Scholar]
  32. Li, Z., Guo, H., Wang, D.X. & Lin, W. (2005) Mesozoic‐Cenozoic tectonic transition in Kuqa Depression‐Tianshan, Northwest China: evidence from Sandstone Detrital and Geochemical Records. Sci. China (Ser. D), 48 (9), 1387–1402.
    [Google Scholar]
  33. Li, Z., Song, W.J., Peng, S.T., Wang, D.X. & Zhang, Z.P. (2004) Mesozoic–Cenozoic tectonic relationships between the Kuqa Subbasin and Tian Shan, northwest China: constraints from depositional records. Sediment. Geol., 172, 223–249.
    [Google Scholar]
  34. Li, Z., Wang, Q., Wang, D., Lin, W. & Wang, Q.C. (2003) Depositional record constraints on Late Cenozoic uplift of Tian Shan and tectonic transformation in Kuqa Subbasin, West China. Acta Sedimentol. Sin., 21 (1), 38–45 (in Chinese with English abstract).
    [Google Scholar]
  35. Liu, C.X., Xu, B.L., Zu, T.R., Lu, F.X., Tong, Y. & Cai, J.H. (2004) Petrochemistry and tectonic significance of Hercynian Alkaline rocks along the Northern margin of the Tarim platform and its adjacent area. Xinjiang Geol., 22 (1), 43–49 (in Chinese with English abstract).
    [Google Scholar]
  36. Liu, H., Wang, Z., Xiong, B., Li, Y., Liu, L.m. & Zhang, J. (2000) Coupling analysis of Mesozoic‐Cenozoic foreland basin and mountain system in central and western China. Earth Sci. Front., 7 (3), 55–72 (in Chinese with English abstract).
    [Google Scholar]
  37. Long, L.L., Gao, J., Xiong, X.M. & Qian, Q. (2006) The geochemical characteristics and the age of the Kule Lake ophiolite in the southern Tianshan. Acta Petrol. Sin., 22 (1), 65–73 (in Chinese with English abstract).
    [Google Scholar]
  38. Long, L.L., Gao, J., Xiong, X.M. & Qian, Q. (2007) Geochemistry and geochronology of granitoids in Bikai region, southern Central‐Tianshan mountains, Xinjiang. Acta Petrol. Sin., 23 (4), 719–732 (in Chinese with English abstract).
    [Google Scholar]
  39. Lu, H., Howell, D.G. & Jia, D. (1994) Rejuvenation of the Kuqa foreland basin, northern flank of the Tarim basin, northwest China. Int. Geol. Rev., 36, 1151–1158.
    [Google Scholar]
  40. Ludwig, K.R. (2003) ISOPLOT 3.0: a geochronological toolkit for Microsoft Excel, Berkeley Geochronology Center. Spec. Pub., 4.
  41. Molnar, P. & Tapponier, P. (1975) Cenozoic tectonics of Asia: effects of a continental collision. Science, 189 (4201), 419–426.
    [Google Scholar]
  42. Nakahjima, T., Uchiumi, S., Maruyama, S., Liou, J.G. & Wang, X. (1990) Evidence for late Proterozoic subduction from 700‐Mya‐old blueschist in China. Nature, 346, 263–265.
    [Google Scholar]
  43. Sengör, A.M.C., Natal’in, B.A. & Burtman, V.S. (1993) Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature, 364, 299–307.
    [Google Scholar]
  44. Sircombe, K.N. (1999) Tracing provenance through the isotope ages of littoral and sedimentary detrital zircon, eastern Australia. Sediment. Geol., 124, 47–67.
    [Google Scholar]
  45. Tapponier, P. & Molnar, P. (1979) Active faulting and Cenozoic tectonics of the Tian Shan, Mongolia and Baykal regions. J. Geophys. Res., 84, 3425–3459.
    [Google Scholar]
  46. Wang, R.S., Wang, Y. & Li, H.M. (1998) Zircon U‐Pb age and its geological significance of high‐pressure terrane of granulite facies in Yushugou area, Southern Tianshan Mountain. Geochimica, 27 (6), 522–527 (in Chinese with English abstract).
    [Google Scholar]
  47. Wiedenbeck, M., Alle, P., Corfu, F., Griffin, W.L., Meier, F., Oberli, F., Von Quadt, A., Roddick, J.C. & Spiegel, W. (1995) Three natural zircon standards for U–Th–Pb, Lu–Hf, trace element, and REE analyses. Geostand. Newslett., 19, 1–23.
    [Google Scholar]
  48. Windley, B.F., Alexeiev, D., Xiao, W., Kroner, A. & Badarch, G. (2007) Tectonic models for accretion of the Central Asian Orogenic Belt. J. Geol. Soc., Lond., 164, 31–47.
    [Google Scholar]
  49. Windley, B.F., Allen, M.B., Zhang, C., Zhao, Z. & Wang, Q. (1990) Paleozoic accretion and Cenozoic redeformation of the Chinese Tien shan Ranges, central Asia. Geology, 18, 128–131.
    [Google Scholar]
  50. Xu, X.Y., Ma, Zh.P., Xia, Z.Ch., Li, X.M. & Wang, L.S. (2006) TIMS U‐Pb isotopic dating and geochemical characteristics of Paleozoic Granitic rocks from the Middle‐Western Section of Tianshan. Northwestern Geol., 39 (1), 50–57 (in Chinese with English abstract).
    [Google Scholar]
  51. Yang, H.B., Gao, P., Li, B. & Zhang, Q.J. (2005) The geological character og thr Sinian Dalubayyi Ophioianshan. Xinjiang. Xinjiang Geol., 23 (2), 123–126. (in Chinese with English abstract).
    [Google Scholar]
  52. Yang, T.N., Li, J.Y., Sun, G.H. & Wang, Y.B. (2006) Earlier Devonian acticve continental arc in Central Tianshan: evidence of geochemical analyses and zircom SHRIMP dating on mylonitized granitic rock. Acta Petrol. Sin., 22 (1), 41–48 (in Chinese with English abstract).
    [Google Scholar]
  53. Yin, A., Nie, S., Craig, P., Harrison, T.M., Ryerson, F.J., Qian, X. & Yang, G. (1998) Late Cenozoic tectonic evolution of the southern Chinese Tian Shan. Tectonics, 17 (1), 1–27.
    [Google Scholar]
  54. Yuan, H.L., Gao, S. & Liu, X.M. (2004) Accurate U‐Pb age and trace element determinations of zircon by laser ablation‐inductively coupled plasma mass spectrometry. Geoanal. Geostand. Res., 28 (3), 353–370.
    [Google Scholar]
  55. Zhang, L.F., Ai, Y.L., Li, Q., Li, X.P., Song, X.G. & Wei, C.J. (2005) The formation and tectonic evolution of UHP metamorphic belt in southwestern Tianshan, Xinjiang. Acta Petrol. Sin., 21 (4), 1029–1038 (in Chinese with English abstract).
    [Google Scholar]
  56. Zhou, D., Graham, S.A., Chang, E.Z., Wang, B. & Hacker, B. (2001) Paleozoic tectonic amalgamation of the Chinese Tian Shan: evidence from a transect along the Dushanzi‐Kuqa Highway. In: Paleozoic and Mesozoic Tectonic Evolution of Central and Eastern Asia: From Continental Assembly to Intracontinental Deformation (Ed. by M.S.Hendrix & G.A.Davis , Geol. Soc. Am. Mem., 194, 23–46.
    [Google Scholar]
  57. Zhou, D.W., Su, L. & Jian, P. (2004) Zircon U‐Pb SHRIMP ages of high‐pressure granulite in Yushugou ophiolitic terrane in southern Tianshan and their tectonic implications. Chin. Sci. Bull., 13, 1411–1415 (in Chinese with English abstract).
    [Google Scholar]
  58. Zhu, Z.X., Wang, K.Zh., Zheng, Y.J., Sun, G.H., Zhang, C. & Li, Y.P. (2006) Zircon SHRIMP dating of Silurian and Devonian granitic intrusions in the southern Yili block, Xinjiang and preliminary discussion on their tectonic setting. Acta Petrol. Sin., 22 (5), 1193–1200 (in Chinese with English abstract).
    [Google Scholar]
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U‐Pb Geochronologic analysis of detrital zircons from the Kuqa Formation (N) sandstone sample. U‐Pb Geochronologic analysis of detrital zircons from the Jidike Formation (N) sandstone sample. U‐Pb Geochronologic analysis of detrital zircons from the Kumugeliemu Formation (E) sandstone sample. U‐Pb Geochronologic analysis of detrital zircons from the Yageliemu Formation (K) sandstone sample. U‐Pb Geochronologic analysis of detrital zircons from the Qiakemake Formation (J) sandstone sample.Please note: Wiley‐Blackwell are not responsible for the content or functionality of any supporting materials supplied by the authors. Any queries (other than missing material) should be directed to the corresponding author for the article.

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