Mesozoic Intra-Continental Progressive Deformation in Western Hunan-Hubei-Eastern Sichuan Provinces of China: Evidence from Apatite Fission Track and Balanced Cross-Section
-
摘要: 从湘鄂西到川东近400 km宽阔的中上扬子陆内中古生界变形是江南—雪峰陆内造山作用向西北方向递进扩展变形的结果.利用磷灰石裂变径迹年龄测定和埋藏热历史模拟以及雪峰山—华蓥山构造剖面的平衡演变分析方法, 揭示出自湘鄂西向川东华蓥山构造变形发展的时代从165 Ma到95 Ma, 具有递进变新的趋势.湘鄂西断褶带厚皮构造变形缩短率小于川东断褶带薄皮构造的变形缩短率, 但侏罗纪时期湘鄂西断褶带的缩短速率却明显大于早白垩世早中时期川东断褶带东南段的缩短速率, 而早白垩世早中时期川东断褶带东南段的缩短速率又大于早白垩世晚期川东断褶带北西段的缩短速率, 反映基底卷入程度和推挤力源的强度大小是控制缩短率和缩短速率的主要原因.这些结果表明湘鄂西—川东中生代陆内变形具有大跨度穿时递进扩展的特征和方式, 并且由于基底的差异和卷入程度的不同以及滑脱层参与深度和程度的不同, 不同构造带缩短率和缩短速率的变化反映出明显的陆内变形及其动力学的差异.研究推测, 如果江南—雪峰隆起是原地或准原地体, 则湘鄂西—川东陆内构造递进扩展变形的"发动机"在桃源—怀化一线, 该线亦是江南—雪峰中生代陆内造山作用开始发轫并向南北两侧呈花状扩展的位置.Abstract: The Mesozoic intra-continental evolution of about 400 km wide middle-upper Yangtze thrust belt from western Hunan-Hubei-eastern Sichuan provinces has been established with a time interval of 70 Ma (from 165 Ma to 95 Ma). Based on apatite fission track (AFT), time-temperature thermal history and balanced cross-section, we conclude that the deformation evolution is progressive from southeast (Jiangnan-Xuefeng intra-continental orogeny) to northwest (Huayingshan thrust belt), and younger and younger. The shortening of thick-skinned fault-fold zone in western Hunan Province-Hubei Province is less than that of thin-skinned fault-fold zone in east Sichuan Province. The shortening rate of the fault-fold zone in western Hunan Province-Hubei Province during Jurassic is obviously more than that of the southeast region of the fault-fold zone of eastern Sichuan Province during the early and middle periods of Early Crataceous. And the shortening rate of the southeast region of the fault-fold zone of eastern Sichuan Province during the early and middle periods of Early Crataceous is more than that of the northwest region of the fault-fold zone of eastern Sichuan Province during the late periods of Early Crataceous. The differences of the shortening rates in the different zones are controlled by the basement and the strength of the compressional deformation. These results indicate that Mesozoic intra-continental deformation in western Hunan Province-Hubei Province to eastern Sichuan Province is progressive with a large width and a long diachronous interval. Because of the different basement, basement involvement level and participation level of detachment layer, the differences of shorterning and shortening rates reflect the obvious differences of intra-continental deformation and its dynamics. The "driving engine" of Mesozoic intra-continental progressive deformation is speculated to be in Taoyuan-Huaihua area, if the Jiangnan-Xuefeng uplift is in place or parautochthon. The Taoyuan-Huaihua area is also where the Jiangnan-Xuefeng Mesozoic intra-continental orogenesis began and expanded southward and northward with a flower-structure geometry.
-
图 1 湘鄂西—川东构造带平面图
Fig. 1. Structural map of the fold belt in western Hunan Province-Hubei Province to eastern Sichuan Province
图 2 湘鄂西—川东构造带平衡演化剖面图
Fig. 2. Balanced cross-sections of the fold belt in western Hunan Province-Hubei Province to eastern Sichuan Province
图 3 湘鄂西—川东构造带典型地层接触关系(点位见图 1)
a.石门雷山洞；b.石门新关；c.龙山北；d.恩施西；e.利川忠路溪；f.宣汉毛坝场东
Fig. 3. Profiles of unconformable contacts in study area
图 5 基于磷灰石裂变径迹分析结果的热历史模拟
1.好的热史范围；2.可以接受的热史范围；3.最佳热史路径
Fig. 5. Time-temperature thermal history modeled based on apatite fission track analyses
表 1 湘鄂西-川东地区磷灰石裂变径迹测定结果
Table 1. Results of AFT of western Hunan Province-Hubei Province to eastern Sichuan Province
样号 构造位置 层位 颗粒数 ρs(Ns)(105/cm) ρi(Ni)(105/cm) P(χ2)(%) t±1σ(Ma) L(μm) n WD-44* 华蓥山背斜 J3 28 1.618(153) 5.699(539) 58.70 47.8±7.1 11.5±1.7 59 WE-8* 万县复向斜 J3 17 3.309(587) 10.186(1 807) 21.52 67.1±4.2 12.3±1.8 101 SJ-2* 方斗山复背斜 J3 16 2.378(264) 6.288(698) 79.41 78.2±6.0 12.0±1.9 74 JL-1* 石柱复向斜 J2 18 5.437(193) 14.535(516) 5.71 76.7±8.8 11.2±2.4 68 X5* 利川复向斜 J2 10 0.699(449) 2.076(1 333) 9.00 61.0±5.1 13.2±0.4 43 Esh-21** 花果坪复向斜 P2 21 25.540(894) 13.770(482) 34.00 154.1±10.2 / / HC-38*** 桑植石门复向斜 S 25 6.963(477) 13.124(899) 45.00 92.0±7.0 11.4±2.3 105 注：ρs和ρi分别表示矿物中自发裂变径迹密度和云母外探测器记录的矿物中诱发裂变径迹密度；Ns和Ni分别表示所测径迹数量；P(χ2)为Chi-sq检验概率，当P(χ2)＞5%时，通常认为所测单颗粒年龄属于同组年龄，否则，属于不同年龄组；t为裂变径迹测定年龄，一般用Central年龄值，当单颗粒年龄为0时，用Pooled年龄值；L为平均径迹长度；n为所测径迹条数.*样品测试由中国科学院高能物理研究所完成；**样品数据苏勇(2007)；***样品数据李双建等(2008). 
下载: 导出CSV
表 2 湘鄂西—川东地区平衡剖面变形量
Table 2. Deformation rate of balanced cross sections of western Hunan Province-Hubei Province to eastern Sichuan Province
时期 剖面位置 变形前剖面长度L0(km) 变形后剖面长度L(km) 缩短量ΔL=L0 —L(km) 缩短率(%)R＝ΔL/L0 侏罗纪末 南东边界断裂—齐岳山 258.3 223.1 35.2 13.6 齐岳山—七里峡 153.9 153.9 0 0 七里峡—华蓥山 52.2 52.2 0 0 早白垩世中期 南东边界断裂—齐岳山 223.1 223.1 0 0 齐岳山—七里峡 153.9 121.3 32.6 21.2 七里峡—华蓥山 52.2 52.2 0 0 早白垩世末 南东边界断裂—齐岳山 223.1 223.1 0 0 齐岳山—七里峡 121.3 121.3 0 0 七里峡—华蓥山 52.2 41.8 10.4 19.9 晚白垩世—古近纪 南东边界断裂—齐岳山 223.1 228.3 -5.2 -2.3 齐岳山—七里峡 121.3 121.3 0 0 七里峡—华蓥山 41.8 41.8 0 0
下载: 导出CSV
表 3 湘鄂西—川东地区平衡剖面缩短速率
Table 3. Shortening rate of balanced cross sections of western Hunan Province-Hubei Province to eastern Sichuan Province
时期 剖面位置 变形时间(起—止)(Ma) 缩短量(km) 缩短率(%) 缩短速率(mm/a) 侏罗纪中晚期 湘鄂西断褶带 20(165~145) 35.2 13.6 1.76 早白垩世早中期 川东断褶带南东段 30(145~115) 32.6 21.2 1.09 早白垩世晚期 川东断褶带北西段 20(115~95) 10.4 19.9 0.52
下载: 导出CSV
-
[1] Artoni, A., Meckel, L.D., 1998. History and deformation rates of a thrust sheet top basin; the Barreme basin, western Alps, SE France (in Cenozoic foreland basins of Western Europe). Geological Society Special Publications, 134: 213-237. doi: 10.1144/GSL.SP.1998.134.01.10 [2] Baudin, T., Marquer, D., Persoz, F., 1993. Basement-cover relationships in the Tambo nappe (Central Alps, Switzerland): geometry, structure and kinematics. Journal of Structural Geology, 15(3-5): 543-553. doi: 10.1016/0191-8141(93)90147-3 [3] Butler, R.W.H., 1987. Thrust sequences. Journal of the Geological Society, 144(4): 619-634. doi: 10.1144/gsjgs.144.4.0619 [4] Cai, L.G., Liu, H.F., 1997. Structural styles and characteristics of fold-thrust belts in Sichuan foreland basin. Experimental Petroleum Geology, 19(2): 115-120 (in Chinese with English abstract). [5] Cai, X.L., Deng, M.S., Wei, X.G., 1993. Analysis of the contact strain of fold structure in Sichuan basin. Journal of Chengdu College of Geology, 20(4): 1-10 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG199304000.htm [6] Charvet, J., Shu, L.S., Shi, Y.S., et al., 1996. The building of South China: collision of Yangzi and Cathaysia blocks, problems and tentative answers. Journal of Southeast Asian Earth Sciences, 13(3-5): 223-235. doi: 10.1016/0743-9547(96)00029-3 [7] Chen, H.H., Sun, S., Li, J.L., et al., 1993. A preliminary study on tectonics of the Xuefeng Mountains, western Hunan. Scientia Geologica Sinica, 28(3): 201-210 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX199303000.htm [8] Chen, M.S., Zhang, S.H., 1998. Characteristics and foming mechanism of opposite protruding arcuate structural zones in the Three Gorges area of the Yangtze River, South China. Geology and Mineral Resources of South China, 1: 47-55 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC199801008.htm [9] Deng, J.F., Zhao, H.L., Mo, X.X., et al., 1995. Intracontinental subduction of the Yangtze continent and continent reducing-inferred from muscovite (two mica) granites. Geological Journal of Universities, 1(1): 50-57 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=GXDX501.005&dbcode=CJFD&year=1995&dflag=pdfdown [10] Ding, D.G., Guo, T.L., Zhai, C.B., et al., 2005. Kink structure in the West Hubei and East Chongqing. Petroleum Geology & Experiment, 27(3): 205-210 (in Chinese with English abstract). [11] Ding, D.G., Liu, G.X., Lü, J.X., et al., 2007. Progressive deformation of Middle Paleozoic marine basins in the Yangtze plate, China. Geological Bulletin of China, 26(9): 1178-1188 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=25447330 [12] Ding, D.G., Zhu, Y., Chen, F.L., et al., 1991. Basal detaching reformation of Paleozoic basins in Central and Lower Yangtze regions and their hydrocarbon prospectings. Oil & Gas Geology, 12(4): 376-386 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT199104002.htm [13] Echavarria, L., Hernández, R., Allmendinger, R., et al., 2003. Subandean thrust and fold belt of northwestern Argentina: geometry and timing of the Andean evolution. AAPG Bulletin, 87(6): 965-985. doi: 10.1306/01200300196 [14] Fan, G.M., 1993. Thrusting nappe-gliding nappe and geological tectonic model in overlying strata of middle section of Jiangnan uplift. Earth Science—Journal of China University of Geosciences, 18(4): 393-402 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX199304002.htm [15] Fan, X.L., 1996. The geological structure of the Xuefeng Mountains-Yuanma basin and its significance to oil exploration. Experimental Petroleum Geology, 18(1): 64-70 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD601.005.htm [16] Feng, X.Y., Meng, X.G., Shao, Z.G., et al., 2001. Deformation features and modeling experiments of nappe/decollement structure in Xuefeng Mountain intracontinental orogenic belt. Acta Geoscientia Sinica, 22(5): 419-424 (in Chinese with English abstract). http://www.oalib.com/paper/1558159 [17] Feng, X.Y., Meng, X.G., Shao, Z.G., et al., 2003. A preliminary discussion on features and dynamics of sequence deformation in South China and neighboring areas. Acta Geoscientia Sinica, 24(2): 115-120 (in Chinese with English abstract). http://www.oalib.com/paper/1559704 [18] Gretener, P.E., 1981. Pore pressure, discontinuities, isostasy and overthrusts. In: McClay, K.R., Price, N.J., eds., Thrust and nappe. Blackwell Scientific Publication, London, 33-39. [19] Guo, A.L., Zhang, G.W., Cheng, S.Y., 2004. Beyond plate tectonics—review on the opportunity for continental geology research. Progress in Natural Science, 14(7): 729-733 (in Chinese). http://www.cqvip.com/QK/96531A/2004007/10010379.html [20] Guo, L.Z., Shi, Y.S., Ma, R.S., et al., 1984. Tectonostratigraphic terranes of Southeast China. Journal of Nanjing University (Natural Sciences), 20(4): 732-739 (in Chinese with English abstract). [21] Guo, Z.W., Deng, K.L., Han, Y.H., et al., 1996. Formation and evolution of Sichuan basin. Geological Publishing House, Beijing (in Chinese). [22] Hindle, D., Besson, O., Burkhard, M., 2000. A model of displacement and strain for arc-shaped mountain belts applied to the Jura arc. Journal of Structural Geology, 22(9): 1285-1296. doi: 10.1016/S0191-8141(00)00038-9 [23] Hossack, J.R., 1983. A cross-section through the Scandinavian Caledonides constructed with the aid of branchline maps. Journal of Structural Geology, 5(2): 103-111. doi: 10.1016/0191-8141(83)90036-6 [24] Hsü, K.J., Sun, S., Li, J.L., et al., 1988. Mesozoic overthrust tectonics in South China. Geology, 16(5): 418-421. doi:10.1130/0091-7613(1988)016<0418:MOTISC>2.3.CO;2 [25] Hu, G.C., Xie, Y.X., 2002. Carboniferous gas fields of steep structural zone in the eastern Sichuan basin, China, Petroleum Industry Press, Beijing (in Chinese). [26] Hu, X.F., 2002. Oil & gas reservoir types in the western region of Hunan and Hubei and exploration orientation. Oil & Gas Geology, 23(3): 300-306 (in Chinese with English abstract). [27] Hu, Z.Q., Zhu, G., Liu, G.S., et al., 2009. The folding time of the eastern Sichuan Jura-type fold belt: evidence from unconformity. Geological Review, 55(1): 32-42 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200901006.htm [28] Huang, J.J., 2000. Research on the stress fields in superposed fold area—an example from northeastern Sichuan. Chinese Journal of Geology (Scientia Geologica Sinica), 35(2): 140-150 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/dzkx200002002 [29] Huang, J.Q., 1954. On major tectonic forms of China. Geological Memoirs, Beijing (in Chinese). [30] Huang, K.N., Opdyke, N.D., 1996. Paleomagnetism of Middle Triassic redbeds from Hubei and northwestern Hunan provinces, South China. Earth and Planetary Science Letters, 143(1-4): 63-79. doi: 10.1016/0012-821X(96)00133-1 [31] Jin, Z.M., Yao, Y.P., 2004. Beyond plate tectonics: What do we do in structural geology? Earth Science—Journal of China University of Geosciences, 29(6): 644-650 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200406001.htm [32] Ketcham, R.A., 2005. Forward and inverse modeling of low-temperature thermochronometry data. Reviews in Mineralogy and Geochemistry, 58: 275-314. doi: 10.2138/rmg.2005.58.11 [33] Ketcham, R.A., Donelick, R.A., Carlson, W.D., 1999. Variability of apatite fission-track annealing kinetics III: extrapolation to geological time scales. American Mineralogist, 84: 1235-1255. doi: 10.2138/am-1999-0903 [34] Laubscher, H.P., 1977. Fold development in the Jura. Tectonophysics, 37(4): 337-362. doi: 10.1016/0040-1951(77)90056-7 [35] Leturmy, P., Mugnier, J.L., Vinour, P., et al., 2000. Piggyback basin development above a thin-skinned thrust belt with two detachment levels as a function of interactions between tectonic and superficial mass transfer: the case of the Subandean Zone (Bolivia). Tectonophysics, 320(1): 45-67. doi: 10.1016/S0040-1951(00)00023-8 [36] Li, B.L., Sun, Y., Chen, W., 1998. Layer gliding systems in eastern Sichuan and their significance for petroleum geology. Oil & Gas Geology, 19(3): 244-261 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT803.012.htm [37] Li, D.W., Zhuang, Y.X., 2006. Scientific problems of continental dynamics in the Qinghai-Tibet plateau. Geological Science and Technology Information, 25(2): 1-10 (in Chinese with English abstract). [38] Li, J.L., Sun, S., Xu, J.H., et al., 1989. New evidences about the evolution of the south Cathay orogenic belt. Chinese Journal of Geology (Scientia Geologica Sinica), 3: 217-225 (in Chinese with English abstract). http://www.researchgate.net/publication/292374965_New_evidence_about_the_evolution_of_the_South_Cathay_orogenic_belt [39] Li, S.J., Xiao, K.H., Wang, X.W., et al., 2008. Thermochronology of detrital minerals in the Silurian strata from southern China and its geological implications. Acta Geologica Sinica, 82(8): 1068-1076 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=DZXE200808007&dbcode=CJFD&year=2008&dflag=pdfdown [40] Li, Z.Q., Ran, L.H., Chen, G.S., et al., 2002. Genetic geologic model and gas-bearing analysis of high and steep structures in East Sichuan. Journal of Chengdu University of Technology, 29(6): 605-609 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=CDLG200206003&dbcode=CJFD&year=2002&dflag=pdfdown [41] Liu, H.F., Liang, H.S., Cai, L.G., et al., 1994. Structural styles of the Longmenshan thrust belt and evolution of the foreland basin in western Sichuan Province, China. Acta Geologica Sinica, 68(2): 101-118 (in Chinese with English abstract). http://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFD&filename=DZXW199404000 [42] Liu, H.F., Liang, H.S., Li, X.Q., et al., 2000. The coupling mechanisms of Mesozoic-Cenozoic rift basins and extensional mountain system in eastern China. Earth Science Frontiers, 7(4): 477-486 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200004015 [43] Liu, L.H., Fang, M.X., Xu, Q., 1999. Structure classification of high and steep structural zones in East Sichuan. Natural Gas Industry, 19(5): 88-90 (in Chinese). [44] Liu, S.G., Wang, Y.C., Zhang, G.X., et al., 1993. The formation mechanism of Dachigan steep structural zone and its effect on the Upper Carboniferous reservoir in the eastern Sichuan basin. Journal of Chengdu Institute of Technology, 21(3): 102-111 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG403.013.htm [45] Ma, R.Y., Peng, J.B., Xi, X.W., et al., 2004. Mechanism of progressive uplift of Qinghai-tibet plateau. Advance in Earth Sciences, 19(Suppl. ): 41-45 (in Chinese with English abstract). [46] Mitra, S., 2003. A unified kinematic model for the evolution of detachment folds. Journal of Structural Geology, 25(10): 1659-1673. doi: 10.1016/S0191-8141(02)00198-O [47] Mugnier, J.L., Huyghe, P., Leturmy, P., et al., 2004. Episodicity and rates of thrust-sheet motion in the Himalayas (western Nepal). AAPG Memoir, 82: 91-114. http://www.researchgate.net/publication/280757260_Episodicity_and_rates_of_thrust_sheet_motion_in_the_Himalayas_western_Nepal_in_McClay_KR_ed_Thrust_tectonics_and_petroleum_systems [48] Qiu, Y.X., Zhang, Y.C., Ma, W.P., 1998. Tectonics and geological evolution of Xuefeng intra-continental orogen, South China. Geological Journal of China Universities, 4(4): 432-443 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX804.007.htm [49] Robinson, D.M., DeCelles, P.G., 2002. Rates of shortening in the Himalayan fold-thrust belt, western Nepal. Abstracts with Programs—Geological Society of America, 34(6): 410. doi: 10.1029/2001TC001322 [50] Shu, L., Charvet, J., 1996. Kinematics and geochronology of the Proterozoic Dongxiang-Shexian ductile shear zone: with HP metamorphism and ophiolitic melange (Jiangnan region, South China). Tectonophysics, 267(1-4): 291-302. doi: 10.1016/S0040-1951C96700104-7 [51] Su, Y., 2007. Tectonic evolution and its controlling effect to hydrocarbon accumulation in western area of Hunan-Hubei (Dissertation). Graduate School of Chinese Aeademy of Sciences, Guangzhou (in Chinese). [52] Tong, C.G., 2000. Relationship between neotectonic movement and structural evolution and gas pools formation of Sichuan basin. Journal of Chengdu University of Technology, 27(2): 123-130 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG200002002.htm [53] Wang, Q., Zhang, P.Z., Niu, Z.J., et al., 2001. Present day crustal movement and tectonic deformation in China continent. Science in China (Series D), 31(7): 529-536 (in Chinese). http://www.onacademic.com/detail/journal_1000035654892810_4312.html [54] Wang, X.L., Zhou, J.C., Qiu, J.S., et al., 2004. Geochemistry of the Meso-to Neoproterozoic basic-acid rocks from Hunan Province, South China: implications for the evolution of the western Jiangnan orogen. Precambrian Research, 135(1-2): 79-103. doi: 10.1016/j.precamres.2004.07.006 [55] Wang, X.Y., Zhu, W.Y., Fu, Y., et al., 2002. Present-time crustal deformation in China and its surrounding regions by GPS. Chinese Journal of Geophysics, 45(2): 198-209 (in Chinese with English abstract). http://www.onacademic.com/detail/journal_1000039162778010_7401.html [56] Wu, G.Y., 2002. The Yanshanian orogeny and Late Mesozoic activation in China continent. Chinese Journal of Geology, 37(4): 453-461 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=DZKX200204008&dbcode=CJFD&year=2002&dflag=pdfdown [57] Xu, J.H., 1989. Geotectonics of South China and the relationship with Japan. Advance in Earth Sciences, 1: 22-27 (in Chinese). [58] Xu, J.H., 1987. It is South China orogen, but not South China platform. Science in China (Series B), 17(10): 1107-1115 (in Chinese). [59] Xu, Y.G., He, Z.A., Wang, J.Y., 2003. A recognition of hydrocarbon potential in western Hunan and Hubei area. Oil & Gas Geology, 24(4): 356-361 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200304009.htm [60] Xu, Z.H., Shi, Y.L., 2003. Lithospheric structure and continental geodynamics. Acta Seismologica Sinica, 25(5): 512-527 (in Chinese with English abstract). [61] Yan, D.P., Wang, X.W., Liu, Y.Y., 2000. Analysis of fold style and it's formation mechanism in the area of boundary among Sichuan, Hubei and Hunan. Geoscience, 14(1): 37-43 (in Chinese with English abstract). http://www.researchgate.net/publication/307557663_Analysis_of_fold_style_and_its_formation_mechanism_in_the_area_of_boundary_among_Sichuan_Hubei_and_Hunan [62] Yan, D.P., Zhou, M.F., Song, H.L., et al., 2003. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze block (South China). Tectonophysics, 361(3-4): 239-254. doi: 10.1016/S0040-1951(02)00646-7 [63] Yang, K.F., Yang, K.G., Ma, C.Q., 2004. Deformation characteristics and ESR dating of Anhua-Xupu fault belt in the Xuefeng Mounatains, Hunan. Geotectonica et Metallogenia, 28(3): 263-269 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical_ddgzyckx-e200501007.aspx [64] Yokoyama, M., Liu, Y.Y., Halim, N., et al., 2001. Paleomagnetic study of Upper Jurassic rocks from the Sichuan basin: tectonic aspects for the collision between the Yangtze block and the North China block. Earth and Planetary Science Letters, 193(3-4): 273-285. doi: 10.1016/S0012-821x(01)00498-8 [65] Yue, G.Y., 1998. Tectonic characteristics and tectonic evolution of Dabashan orogenic belt and its foreland basin. Journal of Mineral. Petrol. , 18(Suppl. )8-15 (in Chinese with English abstract). http://www.researchgate.net/publication/279548447_Tectonic_Characteristics_and_Tectonic_Evolution_of_Dabashan_Orogenic_Belt_and_its_Foreland_Basin [66] Zhang, G.W., Dong, Y.P., Yao, A.P., 2002. Some thoughts on the study of continental dynamics and orogenic belts. Geology in China, 29(1): 7-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200201002.htm [67] Zhang, G.W., Guo, A.L., 2007. Suggestions on enhancing rheological study in structural geology. Chinese Journal of Geology (Scientia Geologica Sinica), 42(1): 10-15 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DZKX200701002.htm [68] Zhang, M.S., Chen, F.J., 1998. Application condition of balanced-section technique and the case analysis. Oil Geophysical Prospecting, 33(4): 532-540, 552 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=SYDQ199804012&dbcode=CJFD&year=1998&dflag=pdfdown [69] Zhao, Z.J., Feng, J.L., Chen, X.S., et al., 2001. Discovery of Dengying Formation fossil pool in Cili, Hunan and its significance. Oil & Gas Geology, 22(2): 114-118 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200102005.htm [70] Zhu, X., Chen, H.J., Sun, Z.C., et al., 1983. The Mesozoic-Cenozoic tectonics and petroliferous basins of China. Acta Geologica Sinica, 3: 235-242 (in Chinese with English abstract). [71] Zoetemeijer, R., Sassi, W., Roure, F., et al., 1992. Stratigraphic and kinematic modeling of thrust evolution, northern Apennines, Italy. Geology, 20: 1035-1038. doi:10.1130/0091-7613(1992)020<1035:SAKMOT>2.3.CO;2 [72] 蔡立国, 刘和甫, 1997. 四川前陆褶皱—冲断带构造样式与特征. 石油实验地质, 19(2): 115-120. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD199702002.htm [73] 蔡学林, 邓明森, 魏显贵, 1993. 四川盆地褶皱构造接触应变分析. 成都地质学院学报, 20(4): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG199304000.htm [74] 陈海泓, 孙枢, 李继亮, 等, 1993. 雪峰山大地构造的基本特征初探. 地质科学, 28(3): 201-210. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX199303000.htm [75] 陈明是, 张树淮, 1998. 长江三峡地区弧形对突构造特征及其形成机制. 华南地质与矿产, 1: 47-55. https://www.cnki.com.cn/Article/CJFDTOTAL-HNKC199801008.htm [76] 邓晋福, 赵海玲, 莫宣学, 等, 1995. 扬子大陆的陆内俯冲与大陆的缩小——由白云母(二云母)花岗岩推导. 高校地质学报, 1(1): 50-57. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX501.005.htm [77] 丁道桂, 郭彤楼, 翟常博, 等, 2005. 鄂西-渝东区膝折构造. 石油实验地质, 27(3): 205-210. doi: 10.3969/j.issn.1001-6112.2005.03.001 [78] 丁道桂, 刘光祥, 吕俊祥, 等, 2007. 扬子板块海相中古生界盆地的递进变形改造. 地质通报, 26(9): 1178-1188. doi: 10.3969/j.issn.1671-2552.2007.09.019 [79] 丁道桂, 朱樱, 陈凤良, 等, 1991. 中、下扬子区古生代盆地基底拆离式改造与油气领域. 石油与天然气地质, 12(4): 376-386. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT199104002.htm [80] 樊光明, 1993. 江南隆起中段盖层中的推覆和滑覆构造及其地质构造模型. 地球科学——中国地质大学学报, 18(4): 393-402. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199304002.htm [81] 范小林, 1996. 雪峰山系-沅麻盆地地质结构及找油意义. 石油实验地质, 18(1): 64-70. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD601.005.htm [82] 冯向阳, 孟宪刚, 邵兆刚, 等, 2001. 雪峰山陆内造山带变形特征及挤压推覆-伸展滑脱构造的物理模拟. 地球学报, 22(5): 419-424. doi: 10.3321/j.issn:1006-3021.2001.05.008 [83] 冯向阳, 孟宪刚, 邵兆刚, 等, 2003. 华南及邻区有序变形及其动力学初探. 地球学报, 24(2): 115-120. doi: 10.3321/j.issn:1006-3021.2003.02.004 [84] 郭安林, 张国伟, 程顺有, 2004. 超越板块构造——大陆地质研究新机遇评述. 自然科学进展, 14(7): 729-733. doi: 10.3321/j.issn:1002-008X.2004.07.002 [85] 郭令智, 施央申, 马瑞士, 等, 1984. 中国东南部地体构造的研究. 南京大学学报(自然科学版), 20(4): 732-739. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ198404014.htm [86] 郭正吾, 邓康龄, 韩永辉, 等, 1996. 四川盆地形成与演化. 北京: 地质出版社. [87] 胡光灿, 谢姚祥, 1997. 中国四川东部高陡构造石炭系气田. 北京: 石油工业出版社. [88] 胡晓凤, 2002. 湘鄂西地区油气藏类型及勘探方向. 石油与天然气地质, 23(3): 300-306. doi: 10.3321/j.issn:0253-9985.2002.03.023 [89] 胡召齐, 朱光, 刘国生, 等, 2009. 川东"侏罗山式"褶皱带形成时代: 不整合面的证据. 地质论评, 55(1): 32-42. doi: 10.3321/j.issn:0371-5736.2009.01.004 [90] 黄继钧, 2000. 纵弯叠加褶皱地区应力场研究——以川东北地区为例. 地质科学, 35(2): 140-150. doi: 10.3321/j.issn:0563-5020.2000.02.002 [91] 黄汲清, 1954. 中国主要地质构造单位. 北京: 地质出版社. [92] 金振民, 姚玉鹏, 2004. 超越板块构造——我国构造地质学要做些什么?地球科学——中国地质大学学报, 29(6): 644-650. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200406001.htm [93] 李本亮, 孙岩, 陈伟, 1998. 川东层滑系统及其油气地质意义. 石油与天然气地质, 19(3): 244-261. doi: 10.3321/j.issn:0253-9985.1998.03.013 [94] 李德威, 庄育勋, 2006. 青藏高原大陆动力学的科学问题. 地质科技情报, 25(2): 1-10, 18. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200602000.htm [95] 李继亮, 孙枢, 许靖华, 等, 1989. 南华夏造山带构造演化的新证据. 地质科学, 3: 217-225. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX198903001.htm [96] 李双建, 肖开华, 汪新伟, 等, 2008. 南方志留系碎屑矿物热年代学分析及其地质意义. 地质学报, 82(8): 1068-1076. doi: 10.3321/j.issn:0001-5717.2008.08.007 [97] 李忠权, 冉隆辉, 陈更生, 等, 2002. 川东高陡构造成因地质模式与含气性分析. 成都理工学院学报, 29(6): 605-609. doi: 10.3969/j.issn.1671-9727.2002.06.003 [98] 刘和甫, 梁慧社, 蔡立国, 等, 1994. 川西龙门山冲断系构造样式与前陆盆地演化. 地质学报, 68(2): 101-118. doi: 10.3321/j.issn:0001-5717.1994.02.001 [99] 刘和甫, 梁慧社, 李晓清, 等, 2000. 中国东部中新生代裂陷盆地与伸展山岭耦合机制. 地学前缘, 7(4): 477-486. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200004025.htm [100] 刘丽华, 范明祥, 徐强, 1999. 川东高陡构造带构造模式分类. 天然气工业, 19(5): 88-90. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG199905023.htm [101] 刘树根, 王允诚, 张高信, 等, 1993. 川东大池干井高陡构造的形成机制及其对石炭系储层的影响. 成都理工学院学报, 21(3): 102-111. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG403.013.htm [102] 马润勇, 彭建兵, 席先武, 等, 2004. 青藏高原的递进式隆升机制. 地球科学进展, 19(增刊): 41-45. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ2004S1007.htm [103] 丘元禧, 张渝昌, 马文璞, 1998. 雪峰山陆内造山带的构造特征与演化. 高校地质学报, 4(4): 432-443. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX804.007.htm [104] 苏勇, 2007. 湘鄂西区块构造演化及其对油气聚集的控制作用(博士论文). 广州: 中国科学院研究生院. [105] 童崇光, 2000. 新构造运动与四川盆地构造演化及气藏形成. 成都理工学院学报, 27(2): 123-130. doi: 10.3969/j.issn.1671-9727.2000.02.003 [106] 王琪, 张培震, 牛之俊, 等, 2001. 中国大陆现今地壳运动和构造变形. 中国科学(D辑), 31(7): 529-536. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200107000.htm [107] 王小亚, 朱文耀, 符养, 等, 2002. GPS监测的中国及其周边现时地壳形变. 地球物理学报, 45(2): 198-209. doi: 10.3321/j.issn:0001-5733.2002.02.006 [108] 吴根耀, 2002. 燕山运动和中国大陆晚中生代的活化. 地质科学, 37(4): 453-461. doi: 10.3321/j.issn:0563-5020.2002.04.009 [109] 许靖华, 1987. 是华南造山带而不是华南地台. 中国科学(B辑), 17(10): 1107-1115. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK198710010.htm [110] 许靖华, 1989. 华南大地构造及其与日本的联系. 地球科学进展, 1: 22-27. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ198901004.htm [111] 徐言岗, 贺自爱, 王津义, 2003. 湘鄂西地区油气前景探析. 石油与天然气地质, 24(4): 356-361. doi: 10.3321/j.issn:0253-9985.2003.04.010 [112] 许忠淮, 石耀霖, 2003. 岩石圈结构与大陆动力学. 地震学报, 25(5): 512-527. doi: 10.3321/j.issn:0253-3782.2003.05.007 [113] 颜丹平, 汪新文, 刘友元, 2000. 川鄂湘边区褶皱构造样式及其成因机制分析. 现代地质, 14(1): 37-43. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200001007.htm [114] 杨奎锋, 杨坤光, 马昌前, 2004. 雪峰山安化-溆浦断裂带变形特征及ESR定年. 大地构造与成矿学, 28(3): 263-269. doi: 10.3969/j.issn.1001-1552.2004.03.006 [115] 乐光禹, 1998. 大巴山造山带及其前陆盆地的构造特征和构造演化. 矿物岩石, 18(增刊): 8-15. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS8S1.001.htm [116] 张国伟, 董云鹏, 姚安平, 2002. 关于中国大陆动力学与造山带研究的几点思考. 中国地质, 29(1): 7-13. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200201002.htm [117] 张国伟, 郭安林, 2007. 关于加强流变构造学研究的建议. 地质科学, 42(1): 10-15. doi: 10.3321/j.issn:0563-5020.2007.01.002 [118] 张明山, 陈发景, 1998. 平衡剖面技术应用的条件及实例分析. 石油地球物理勘探, 33(4): 532-540, 552. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ199804012.htm [119] 赵宗举, 冯加良, 陈学氏, 等, 2001. 湖南慈利灯影组古油藏的发现及意义. 石油与天然气地质, 22(2): 114-118. doi: 10.3321/j.issn:0253-9985.2001.02.006 [120] 朱夏, 陈焕疆, 孙肇才, 等, 1983. 中国中、新生代构造与含油气盆地. 地质学报, 3: 235-242. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198303002.htm -
点击查看大图
图(5) / 表(3)
计量
- 文章访问数: 3758
- HTML全文浏览量: 183
- PDF下载量: 114
- 被引次数: 0
