The coupling relationship between the west Shandong rise and the Jiyang depression, China

Abstract

This article reports 21 AFT (apatite fission track) data from the West Shandong (山东) rise (WSR) and Jiyang (济阳) depression, and mainly studies their Cenozoic uplifting/subsidence history and the relationship between them. Furthermore, we improve our insights into the Bohai Bay Basin (BBB). Our AFT analysis and AFT T-t modeling indicates that the WSR was uplifted at ca. 65 Ma with apparent uplift rate of 0.019 mm/a; it underwent two relatively rapid uplifting events at 43–33 and 16–0 Ma with rates of 0.097 and 0.052 mm/a, respectively. Meanwhile, the Jiyang depression subsided at rate of 0.032 mm/a at 52–43 Ma, and the rate increased to 0.13 mm/a at ca. 42–33 Ma; finally the subsidence rate increased to 0.053 mm/a in 16–0 Ma. They all underwent a uplift in time of 23–16 Ma with rate of 0.04–0.07 mm/a. A careful comparison shows that the Cenozoic uplifting of the WSR coupled well with the subsidence of the Jiyang depression. Our research also suggests that the uplift-basin coupling events are part of the couplings between the Bohai Bay Basin and its peripheral mountains. This intraplate mountain-basin coupling is a reflection of global tectonic events.

Keywords

AFT / tectonic uplift-denudation / subsidence / coupling relationship / western Shandong rise / Jiyang depression

References

[1] Ai X S, Zhang C J, Wang S J. Progress in Regional Geological Surveys in Shandong Province over the Past Ten Years. Regional Geology of China, 1998, 17(3): 228-235.

[2] Boyer S E. Sedimentary Basin Taper as a Factor Controlling the Geometry and Advance of Thrust Belts. American Journal of Science, 1995, 295: 1220-1254.

[3] Brandon M T. BINOMFIT: A Windows Program for Estimating Fission-Track Ages for Concordant and Mixed Grain Age Distributions, 2002, 1-11.

[4] Brown R W, Summerfield M A, Gleadow A J W. Kirkby M J. Apatite Fission Track Analysis: Its Potential for the Estimation of Denudation Rates and Implications for Models of Long Term Landscape Development. Process Models and Theoretical Geomorphology, 1994 Chichester: John Wiley & Sons, 23-53.

[5] Cai J G. Evaluation of Sedimental Source in Dongying Dustpan Like Rift. Petroleum Geology and Recovery Efficiency, 2001, 8(6): 5-8.

[6] Chen A D. Dynamic Mechanism of Formation of Dustpan Subsidence, Northern Jiangsu. Geological Journal of China Universities, 2001, 7(4): 408-418.

[7] Chen J S. Features of the Jiyang Movement and Its Effects on the Evolution of the Jiyang Depression. Experimental Petroleum Geology, 1993, 15(1): 86-99.

[8] Chi P X, Luan H Y, Liu M W, . On the Division and Correlation of the Cenozoic Lithostratigraphic Units in Shandong Province. Geology of Shandong, 1994, 10(S1): 70-86.

[9] Copeland P, Harrison T M, Pan Y, . Thermal Evolution of the Gangdese Batholith, Southern Tibet: A History of Episodic Unroofing. Tectonics, 1995, 14: 223-236.

[10] Davis D, Suppe J, Dahlen F A. Mechanics of Folds and Thrust Belts and Accretionary Wedges. Journal of Geophysical Research, 1983, 88(B2): 1153-1172.

[11] Davis G A, Qian X, Zheng Y, . Yin A, Harrison M, . Mesozoic Deformation and Plutonism in the Yunmeng Shan: A Chinese Metamorphic Core Complex North of Beijing, China. the Tectonic Evolution of Asia, 1996 Cambridge: Cambridge University Press, 253-280.

[12] Duan J Y, Liu P J, Xia D X. The Preliminary Research on Tectonic Pattern and Tectonic Evolution of Mesoproterozoic-Paleozoic in North China Plate. Geoscience, 2002, 16(4): 333-338.

[13] Foster D A, Gleadow A J W. The Morphotectonic Evolution of Rift-Margin Mountains in Central Kenya: Constraints from Apatite Fission Track Analysis. Earth and Planetary Science Letters, 1992, 113: 157-171.

[14] Galbraith R F. On Statistical Methods: What are the Real Alternatives?. Mathematic Geology, 1981, 13: 471-478.

[15] Gallagher K, Brown R P. The Onshore Record of Passive Margin Evolution. Journal of the Geological Society, 1997, 154(3): 451-457.

[16] Gallagher K, Brown R W, Johnson C. Fission Track Analysis and Its Applications to Geological Problems. Annual Reviews of Earth and Planetary Sciences, 1998, 26: 519-572.

[17] Gleadow A J W. Fission Track Dating Methods: What are the Real Alternatives?. Nuclear Tracks Radiation Measurement, 1981, 5: 3-14.

[18] Gleadow A J W, Brown R W. Summerfield M A. Fission Track Thermochronology, and the Long-Term Denudation Response to Tectonics. Geomorhpology and Global Tectonics, 2000 Chichester: John Wiley and Sons Lts., 57-75.

[19] Gleadow A J W, Dubby I R, Lovering J F. Confined Fission Track Lengths in Apatite: A Diagnostic Tool for Thermal History Analysis. Contributions to Mineralogy and Petrology, 1986, 94: 405-415.

[20] Gleadow A J W, Duddy I R. Natural Long-Term Annealing Experiment for Apatite. Nuclear Tracks and Radiation Measurements, 1981, 5: 169-174.

[21] Green P F. The Relationship between the Track Shortening and Fission Track Age Reduction in Apatite; Combined Influences of Inherent Instability, Annealing Anisotropy, Length Bia and System Calibration. Earth and Planetary Science Letters, 1988, 89: 335-352.

[22] Green P F, Duddy I R, Gleadow A J W, . Thermal Annealing of Fission Tracks in Apatite; 1, A Qualitative Description. Chemical Geology, 1986, 59: 236-253.

[23] Green P F, Duddy I R, Laslett G M, . Thermal Annealing of Fission Tracks in Apatite; 4, Qualititave Modeling Techniques and Extensions to Geological Timescales. Chemical Geology, 1989, 79: 155-182.

[24] Guo S P, Shi X B, Wang L S. Thermal History Analysis of Dongying Depression, Shengli Oil Region. Oil and Gas Geology, 1996, 17(1): 32-36.

[25] Han D L, Li Z, Li S Y, . Geochemical Characteristics of Paleogene Mudstones in the Bo’xing Sag, North of the West Shandong Rise, and Their Tectonic Implications. Chinese Journal of Geology, 2007, 42(4): 678-689.

[26] Harrison T M, Copeland P, Kjdd W S F, . Raising Tibet. Science, 1992, 255: 1663-1670.

[27] He B. On Dynamics of the Bohai Bay Complex Faulted Basin. Experimental Petroleum Geology, 2001, 23(1): 27-30.

[28] Hendrix M S, Dumitru T A, Graham S A. Late Oligocene-Early Miocene Unroofing in the Chinese Tian Shan: An Early Effect of the India-Asia Collision. Geology, 1994, 22: 487-490.

[29] Hu J Y, Niu J Y. The Further Deepening of Oil-Gas Accumulation Theory and Exploratory Practice of Bohai Bay Basin. Acta Petrolei Sinica, 2001, 22(1): 1-5.

[30] Hurford A J. Standardization of Fission Track Dating Calibration: Recommendation by the Fission Track Working Group of the IUGS Subcommission on Geochronology. Chemical Geology, 1990, 80: 171-178.

[31] Hurford A J, Green P F. The Zeta Age Calibration of Fission-Track Dating. Chemical Geology, 1983, 41: 285-317.

[32] Jolivet L, Tamaki K, Fournier M. Japan Sea, Opening History and Mechanism: A Synthesis. Journal of Geophysical Research, 1994, 99(B11): 22237-22259.

[33] Ketcham R A. Forward and Inverse Modeling of Low-Temperature Thermochronometry Data. Reviews in Mineralogy and Geochemistry, 2005, 58: 275-314.

[34] Ketcham R A, Donelick R A, Carlson W D. Variability of Apatite Fission-Track Annealing Kinetics: III. Extrapolation to Geological Time Scales. American Mineralogist, 1999, 84: 1235-1255.

[35] Laslett G M, Green P F, Duddy I R, . Thermal Annealing of Fission Tracks in Apatite; 2. A Quantitative Description. Chemical Geology, 1987, 65: 1-13.

[36] Li L, Dai J S. Numerical Simulation of Tectonics Stress Field and Fracture Distribution of Mesozoic and Paleozoic Erathem in Chendao Area. Jouranl of University of Petroleum, China., 2000, 24(1): 6-9.

[37] Li L, Zhong D L. Fission Track Evidence of Cenozoic Uplifting Events of the Taishan Mountain, China. Acta Petrologica Sinica, 2005, 22(2): 457-464.

[38] Li L, Zhong D L, Shi X P, . Late Mesozoic-Cenozoic Décollement Structure and Its Deep Geological Background in Western Shandong, China. Progress in Natural Science, 2009, 19: 603-613.

[39] Li S Z, Suo Y H, Dai L M, . Development of the Bohai Bay Basin and destruction of the North China Craton. Earth Science Frontiers, 2010, 17(4): 64-89.

[40] Li Z, Xu C W, Shi Y H, . Discovery of Detrital High-Pressure Metamorphic Minerals from Paleocene-Eocene Strata in Jiyang Depression, Eastern North China, and Its Implication for Tectonic-Paleogeographic Setting. Acta Petrologica Sinica, 2009, 25(12): 3130-3140.

[41] Liu H F, Liang H S, Li X Q, . The Coupling Mechanisms of Mesozoic-Cenozoic Rift Basins and Extensional Mountain System in Eastern China. Earth Science Frontiers, 2000, 7(4): 477-486.

[42] Liu M, Cui X J, Liu F T. Cenozoic Rifting and Volcanism in Eastern China: A Mantle Dynamic Link to the Indo-Asia Collsion?. Tectonophisics, 2004, 393: 29-42.

[43] Liu Z L. Dynamic Systems for Pool Formation of the Chezhen Sag. Northwestern Gology, 2004, 37(4): 22-26.

[44] Lu K Z, Qi J F. The Cenozoic Tectonic Models of the Bohai Bay Basin, 1997 Beijing: Geological Press

[45] Ma X Y, Liu H F, Wang W X, . Meso-Cenozoic Taphrogeny and Extensional Tectonics in Eastern China. Acta Geologica Sinica, 1983, 57(1): 22-31.

[46] Ma Y S, Cui S Q, Wu G G, . Uplift History of the Yiwulushan Mountain in West Liaoning. Acta Geoscientia Sinica, 2000, 21(3): 245-253.

[47] Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific Plate Relative to Eurasia and Its Potential Relation to Cenozoic Extension along the Eastern Margin of Eurasia. Geology, 1995, 23(8): 719-722.

[48] O’Sullivan P B, Foster D A, Kohn B P, . Multiple Post Orogenic Denudation Events: An Example from the Eastern Lachlan Fold Belt. Australia Geology, 2000, 24(6): 563-566.

[49] Patriat P, Achache J. India Eurasia Collision Chronology has Implications for Crustal Shortening and Driving Mechanism of Plates. Nature, 1984, 311: 615-621.

[50] Qiu N S, Li S P, Zeng J H. Thermal History and Tectonic-Thermal Evolution of the Jiyang Depression in the Bohai Bay Basin, East China. Acta Geologica Sinica, 2004, 78(2): 263-269.

[51] Ren Z L. Comparative Research on Tectonical Thermal History of Sedimentary Basins in the North China: [Dissertation], 1998 Xi’an: Northwest University

[52] Schärer U, Zhang L, Tapponnier P. Duration of Strike-Slip Movements in Large Shear Zones, the Red River Belt, China. Earth and Planetary Science Letters, 1994, 126: 379-397.

[53] Shi B Q, Wu Z P, Wang J X, . A Study on the Geological Characteristics and Geodynamic Origin of Dongying Movement, Bohia Bay Basin. Experimental Petroleum Geology, 1999, 21(3): 196-200.

[54] Shi B Q, Zheng F Y, Zhou Y Q, . A Study on the Geological Characteristics and Geodynamic Origin of Jiyang Movement, Bohia Bay Basin. Geological Journal of China Universities, 2002, 8(3): 356-363.

[55] Shi Y H, Zhu G, Wang D X. Metamorphic P-T Evolution for the Garnet Amphibolite from Feidong Group in the South of Zhangbaling Uplift across Tan-Lu Fault and Its Influence on Tectonics. Acta Petrologica Sinica, 2009, 25(12): 3335-3345.

[56] Shuai D F, Wang B H. Petroleum Geology of China—Vol.6, Shengli Oil Field, 1987 Beijing: Editional Committee of “Petroleum Geology of China”. Petroleum Industry Press

[57] Song D N. Basic Characteristics and Evolution History of Meso-Cenozoic Basins in Shandong Province. Geology of Shandong, 2001, 17(5): 5-17.

[58] Song M S. Mesozoic and Cenozoic Maturity Curve of Jiyang Depression and Its Application in Calculation of Strata Denudation. Geological Journal of China Universities, 2004, 10(1): 121-127.

[59] The Fourth GeologyMineral Institute of Shandong Province Regional Geology of Shandong Province, 2003 Jinan: Map Press of Shandong Province

[60] Wang B H, Qian K. Geological Research and Oil-Gas Exploration in Shengli Oilfield, 1992 Dongying: China University of Petroleum Press

[61] Wernicke B. Low Angle Normal Faults in the Basin and Range Province: Nappe Tectonics in an Extending Orogen. Nature, 1981, 291: 645-648.

[62] Wu F D, Chen J Y, Liu C Y, . Tertiary Sequence Stratigraphic Framework and Sedimentary System Types in Dongying Depression. Geoscience, 1998, 12(4): 559-566.

[63] Xu J W, Zhu G, Tong W X, . Formation and Evolution of the Tancheng-Lujiang Wrench Fault System: A Major Shear System to the Northwest of the Pacific Ocean. Tectonophysics, 1987, 134: 273-310.

[64] Xu W L, Le J Y. Tectonic Movement and Evolution of the East China Sea. Marine Geology and Quaternary Geology, 1988, 8(1): 9-21.

[65] Yan D S, Wang S W, Tang Z. The Block Activity and the Forming of Paleo-Burried Hill Reservoir in Bohai Bay Basin. Acta Petrolei Sinica, 1980, 1(2): 1-10.

[66] Zeitler P K. Cooling History of NW Himalaya, Pakinstan. Tectonics, 1985, 4: 127-151.

[67] Zhang J S, Zhang J S, Xu J, . Meso-Cenozoic Détachment Zones in the Front of the Taihang Mountains and Their Fission-Track Ages. Geological Bulletin of China, 2002, 21(4–5): 207-210.

[68] Zhang M L, Jin Z J, Lü P J, . Formation of Taishan Moumtain and Cenozoic Tectonicism. Journal of Geomechanic, 2000, 6(2): 23-29.

[69] Zhong D L. The Paleotethys Orogenic Belts of the Western Yunnan and Sichuan Province, 1998 Beijing: Scientific Publishing House

[70] Zhong D L, Ding L. Rising Process of the Qinghai-Xizang (Tibet) Plateau and Its Mechanism. Science in China Series D: Earth Sciences, 1996, 39(4): 369-379.

[71] Zong G H, Xiao H Q, Li C B, . Evolution of Jiyang Depression and Its Tectonic Implications. Geological Journal of China Universities, 1999, 5(3): 275-282.