Middle Jurassic Folds in Northern Lianhuashan Fault Zone in Guangdong Province and Its Tectonic Significance
-
摘要: 为限定华南东部沿海中生代褶皱的形成时代，研究其形成机制，以广东莲花山断裂带北段晚三叠世至中侏罗世地层褶皱为研究对象，进行了构造解析和相关地质体的年代学分析.地层产出的蕨类、篦羽叶和双壳类等化石，证实其晚三叠世至中侏罗世的沉积时代.NE向褶皱被晚侏罗世火山岩（锆石U-Pb年龄163~148 Ma）不整合覆盖，NW向褶皱被晚侏罗世花岗岩（锆石U-Pb年龄157~154 Ma）侵入，综合前人在地层中获取的碎屑锆石最新U-Pb年龄（171~173 Ma），分析显示褶皱于中侏罗世中晚期近同期形成.NE向褶皱为纵弯褶皱，形成于NW-SE向区域性挤压作用；NW向褶皱为剪切褶皱，受控于褶皱逆冲带中NW向横断层作用.广东莲花山断裂北段中侏罗世不同走向褶皱均是华南板块对古太平洋板块俯冲的响应.Abstract: In order to limit the timing of Mesozoic folds in the eastern coast of South China and study the formation mechanism, in this paper it studies the folds of the Late Triassic to Middle Jurassic strata in the northern section and analyzes the geochronology of related geological bodies. Fossils of ferns, pinnules, bivalves found in the strata confirm the sedimentary age from the Late Triassic to the Middle Jurassic. The NE fold is invaded by the Late Jurassic volcanic rock (zircon U-Pb age at 163-148 Ma). The NW fold is invaded by the Late Jurassic granite (zircon U-Pb age at 157-154 Ma). Combined with the previous debris zircon U-Pb age obtained in the formation (171-173 Ma), comprehensive analysis indicates that the fold was formed in the middle and late Middle Jurassic. NE fold is longitudinal bending fold, which is the product of regional NW-SE extrusion; NW fold is formed by shear fold, which is the product of NW transverse fault in the fold reverse zone. The different trending Jurassic folds in the northern section of Lianhuashan fault, Guangdong, are the tectonic response of South China block to the subduction of the Paleo-Pacific plate.
-
图 1 地质背景及采样位置
a.广东莲花山断裂带北段简要地质图；b.中生代沉积岩浆建造及采样层位.1.下白垩统碎屑岩；2.上侏罗统‒下白垩统火山岩；3.中侏罗统碎屑岩；4.下侏罗统碎屑岩；5.上三叠统碎屑岩；6.中新元古代变质地层；7.晚侏罗世‒早白垩世花岗岩；8.三叠纪花岗岩；9.奥陶纪‒志留纪花岗岩；10.正断层（°）；11.走滑断层（°）；12.逆断层（°）；13.背斜/向斜；14.图 2剖面位置；15.岩浆岩锆石U-Pb测年采样位置及编号；16.古生物化石采样位置及编号；17.碎屑锆石U-Pb测年采样位置（Zhang et al.，2019/Xu et al.，2019）
Fig. 1. Geological background and sampling locations
图 2 梅县南九龙嶂复式向斜北西翼略图
据广东1∶5万畲坑圩幅、水车圩幅、五华县幅、丰良镇幅区域地质调查报告. 1.早白垩世花岗岩；2.下侏罗统桥源组；3.冲积物；4.粉砂岩；5.炭质泥岩；6.长石石英砂岩；7.黑云母二长花岗岩；8.花岗斑岩；9.逆断层；10.正断层；11.推测断层
Fig. 2. Section of the west wing of Jiulongzhang synclinore in southern Meixian City
图 3 晚三叠世‒中侏罗世碎屑岩层野外照片与产状特征
a，b.野外测量NE向褶皱层面产状；c，d.野外测量NW向褶皱层面产状
Fig. 3. Field photos and attitude characteristics of the Late Triassic-Middle Jurassic clastic rock formation
图 4 晚三叠‒中侏罗世地层产状统计（下半球等面积赤平投影）
a.所有地层产状；b.NE-SW向地层产状与π图解；c.NW-SE向地层产状与π图解
Fig. 4. Attitude statistics of Late Triassic-Middle Jurassic strata (stereographic projection in the lower hemisphere)
图 5 代表性植物化石
a.裂页爱博拉契蕨，相似种Eboracia cf. lobifolia（Phillips）Thomas；b.枝脉蕨，未定种Cladophlebis sp.；c.连平奇叶蕨，相似种Thaumatopteria cf lianpingensis Liu；d.爱博拉契蕨，未定种Eboracia sp.；e.类紫萁，未定种Osmundopsis sp.；f.日本篦羽叶，相似种Ctenis cf.japonica Oishi
Fig. 5. Typical plant fossils
图 7 代表性双壳类化石
a.卵型湖南蛤Hunanella ovata Xiong et Wang；b. 卵形湖南蛤，相似种Hunanella cf. ovate Xiong et Wang；c. 长形湖南蛤，相似种Hunanella cf. longa Xiong et Wang；d. 楔形醴陵蛤，相似种Lilingella cf.cuneata Wu；e. 粗壮醴陵蛤，相似种Lilingella cf. robusta Zhou；f. 新余醴陵蛤，相似种Lilingella cf. xinyunensis Xiong et Wang
Fig. 7. Typical fossils of bivalves
图 8 坪沙花岗岩和热水洞组（J3r）火山岩锆石U-Pb年龄谐和图
Fig. 8. U-Pb concordia plots for zircons from Pingsha granite and Reshuidong Formation (J3r)
图 9 碎屑锆石年龄谱指示的沉积构造背景
底图据Cawood et al.，2012；锆石U-Pb年龄数据引自Xu et al.，2019；Zhang et al.，2019
Fig. 9. Tectonic background indicated by detrital zircon age spectra
表 1 坪沙花岗岩和热水洞组（J3r）锆石U-Pb测年数据
Table 1. Data of zircon U-Pb dating of Pingsha granite and Reshuidong Formation(J3r)
样品编号
及测点序号Th(10‒6) U(10‒6) Th/U 207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238U207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238URatio 1sigma Ratio 1sigma Ratio 1sigma 年龄(Ma) 1sigma 年龄(Ma) 1sigma Age (Ma) 1sigma LHS-06 热水洞组（J3r） 1 138 331 0.4 0.047 146 0.002 673 0.149 743 0.007 936 0.023 194 0.000 322 58 130 142 7 148 2 2 335 867 0.4 0.047 997 0.001 735 0.156 060 0.005 407 0.023 614 0.000 236 98 88 147 5 150 1 3 466 702 0.7 0.052 179 0.001 818 0.180 792 0.006 055 0.025 194 0.000 334 300 80 169 5 160 2 4 35 61 0.6 0.053 176 0.006 357 0.253 079 0.014 557 0.023 395 0.000 622 345 274 229 12 149 4 5 615 1 969 0.3 0.049 936 0.001 056 0.275 337 0.006 084 0.039 778 0.000 375 191 48 247 5 251 2 6 289 410 0.7 0.045 302 0.002 129 0.142 137 0.006 469 0.022 881 0.000 293 error 135 6 146 2 7 256 401 0.6 0.050 917 0.002 653 0.161 379 0.007 741 0.022 968 0.000 338 235 116 152 7 146 2 8 263 602 0.4 0.047 705 0.001 915 0.158 571 0.005 867 0.023 894 0.000 305 83 93 149 5 152 2 9 309 745 0.4 0.048 179 0.001 614 0.152 470 0.004 877 0.022 966 0.000 252 109 77 144 4 146 2 10 230 395 0.6 0.050 116 0.002 915 0.163 265 0.009 605 0.023 670 0.000 317 211 135 154 8 151 2 11 269 736 0.4 0.050 670 0.001 773 0.159 983 0.005 710 0.022 766 0.000 221 233 81 151 5 145 1 12 412 774 0.5 0.052 492 0.002 019 0.167 043 0.005 939 0.023 296 0.000 287 306 87 157 5 148 2 13 336 645 0.5 0.050 008 0.002 243 0.155 576 0.006 555 0.022 662 0.000 249 195 106 147 6 144 2 14 65 133 0.5 0.057 953 0.005 268 0.214 138 0.013 847 0.022 608 0.000 459 528 197 197 12 144 3 15 125 291 0.4 0.054 114 0.003 329 0.168 038 0.009 554 0.023 151 0.000 374 376 139 158 8 148 2 16 963 608 1.6 0.049 770 0.002 278 0.150 217 0.006 555 0.021 783 0.000 269 183 107 142 6 139 2 17 161 335 0.5 0.055 213 0.003 081 0.177 065 0.009 662 0.023 121 0.000 287 420 121 166 8 147 2 18 325 414 0.8 0.052 298 0.002 682 0.167 527 0.007 791 0.022 934 0.000 321 298 119 157 7 146 2 19 594 1 212 0.5 0.049 986 0.002 000 0.160 510 0.006 461 0.023 200 0.000 230 195 93 151 6 148 1 20 65 100 0.6 0.064 108 0.005 935 0.246 896 0.012 811 0.022 066 0.000 489 746 165 224 10 141 3 样品编号
及测点序号Th(10‒6) U(10‒6) Th/U 207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238U207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238URatio 1sigma Ratio 1sigma Ratio 1sigma Age (Ma) 1sigma Age (Ma) 1sigma Age (Ma) 1sigma LHS-07 热水洞组（J3r） 1 191 487 0.4 0.049 669 0.002 123 0.161 783 0.006 940 0.023 570 0.000 288 189 100 152 6 150 2 2 248 679 0.4 0.046 347 0.001 737 0.155 089 0.006 068 0.024 118 0.000 261 17 85 146 5 154 2 3 520 712 0.7 0.050 436 0.001 913 0.168 600 0.006 539 0.024 162 0.000 320 217 89 158 6 154 2 4 225 590 0.4 0.045 014 0.001 942 0.147 260 0.006 392 0.023 622 0.000 278 error 139 6 151 2 5 312 729 0.4 0.048 705 0.001 877 0.154 936 0.005 879 0.023 124 0.000 281 200 91 146 5 147 2 6 171 462 0.4 0.050 808 0.002 224 0.160 220 0.007 118 0.022 835 0.000 259 232 102 151 6 146 2 7 219 522 0.4 0.046 851 0.001 937 0.154 342 0.006 411 0.023 824 0.000 312 43 157 146 6 152 2 8 160 458 0.4 0.048 823 0.002 321 0.159 039 0.007 427 0.023 599 0.000 296 139 111 150 7 150 2 9 749 1 421 0.5 0.047 416 0.001 455 0.157 218 0.004 672 0.024 043 0.000 255 78 65 148 4 153 2 10 233 623 0.4 0.050 983 0.002 369 0.168 957 0.007 656 0.024 080 0.000 243 239 107 159 7 153 2 11 161 477 0.3 0.049 034 0.002 233 0.156 884 0.007 081 0.023 231 0.000 277 150 107 148 6 148 2 12 220 634 0.3 0.054 915 0.002 272 0.184 822 0.007 912 0.024 237 0.000 292 409 88 172 7 154 2 13 255 535 0.5 0.047 790 0.002 254 0.158 156 0.007 117 0.023 813 0.000 317 87 111 149 6 152 2 14 234 1 103 0.2 0.049 480 0.001 560 0.160 578 0.005 002 0.023 532 0.000 231 172 74 151 4 150 1 15 280 706 0.4 0.047 954 0.001 817 0.151 976 0.005 804 0.022 947 0.000 239 98 ‒108 144 5 146 2 16 252 478 0.5 0.052 246 0.002608 0.164 696 0.007 608 0.023 117 0.000 337 295 108 155 7 147 2 17 202 581 0.3 0.051 744 0.002427 0.162 555 0.007 389 0.022 900 0.000 257 272 114 153 6 146 2 18 404 791 0.5 0.046 137 0.001622 0.148 202 0.005 157 0.023 201 0.000 213 400 ‒313 140 5 148 1 19 453 770 0.6 0.050 921 0.001920 0.169 750 0.006 516 0.024 161 0.000 293 239 87 159 6 154 2 20 259 473 0.5 0.048 767 0.002342 0.158 143 0.007 887 0.023 644 0.000 367 200 118 149 7 151 2 样品编号
及测点序号Th(10‒6) U(10‒6) Th/U 207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238U207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238URatio 1sigma Ratio 1sigma Ratio 1sigma Age (Ma) 1sigma Age (Ma) 1sigma Age (Ma) 1sigma D6208 坪沙花岗岩体 1 1 426 18 263 0.1 0.049 019 0.001 350 0.166 536 0.004 534 0.024 751 0.000 303 150 65 156 4 158 2 2 834 2 975 0.3 0.058 976 0.002 248 0.205 558 0.008 969 0.024 991 0.000 318 565 88 190 8 159 2 3 1 294 4 021 0.3 0.131 070 0.006 823 0.459 560 0.024 380 0.025 042 0.000 527 2 122 96 384 17 159 3 4 1 225 3 614 0.3 0.053 162 0.001 721 0.179 153 0.005 717 0.024 561 0.000 290 345 74 167 5 156 2 5 1 529 17 395 0.1 0.053 398 0.001 467 0.180 558 0.005 004 0.024 556 0.000 291 346 61 169 4 156 2 6 603 846 0.7 0.049 977 0.002 039 0.288 359 0.011 194 0.041 955 0.000 647 195 96 257 9 265 4 7 1 268 6 414 0.2 0.049 952 0.001 709 0.162 836 0.005 460 0.023 679 0.000 259 195 106 153 5 151 2 8 608 1 020 0.6 0.105 234 0.004 460 0.356 824 0.015 198 0.024 656 0.000 334 1 718 78 310 11 157 2 9 1 133 3 301 0.3 0.063 375 0.002 926 0.213 375 0.009 502 0.024 530 0.000 278 720 98 196 8 156 2 10 97 151 0.6 0.053 437 0.005 457 0.253 073 0.013 840 0.023 798 0.000 635 346 233 229 11 152 4 11 626 1 131 0.6 0.048 593 0.002 570 0.168 483 0.008 476 0.024 756 0.000 319 128 128 158 7 158 2 12 1 371 13 272 0.1 0.049 485 0.001 509 0.169 798 0.005 118 0.024 805 0.000 292 172 70 159 4 158 2 13 91 131 0.7 0.058 607 0.008 873 0.308 749 0.028 237 0.024 200 0.000 765 554 335 273 22 154 5 14 437 1 276 0.3 0.047 676 0.001 886 0.160 408 0.006 296 0.024 389 0.000 307 83 93 151 6 155 2 15 126 154 0.8 0.050 217 0.005 727 0.234 032 0.014 048 0.023 262 0.000 620 206 244 214 12 148 4 16 629 1 893 0.3 0.056 487 0.002 300 0.204 976 0.008 602 0.026 059 0.000 314 472 89 189 7 166 2 17 3 444 10 969 0.3 0.093 050 0.004 005 0.323 756 0.013 636 0.025 120 0.000 291 1 500 81 285 10 160 2 18 684 4 575 0.1 0.047 747 0.001 521 0.167 865 0.005 294 0.025 297 0.000 277 87 76 158 5 161 2 19 1 408 3 827 0.4 0.059 605 0.002 219 0.202 021 0.007 628 0.024 281 0.000 252 591 114 187 6 155 2 20 1 161 3 462 0.3 0.294 483 0.010 652 1.604 647 0.078 913 0.037 475 0.000 789 3 442 57 972 31 237 5 样品编号
及测点序号Th(10-6) U(10‒6) Th/U 207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238U207Pb/
206Pb207Pb/
206Pb207Pb/
235U207Pb/
235U206Pb/
238U206Pb/
238URatio 1sigma Ratio 1sigma Ratio 1sigma Age (Ma) 1sigma Age (Ma) 1sigma Age (Ma) 1sigma D6213 坪沙花岗岩体 1 1 334 10 574 0.1 0.049 281 0.001 412 0.177 337 0.005 170 0.025 819 0.000 320 161 64 166 4 164 2 2 208 291 0.7 0.055 333 0.004 251 0.212 519 0.012 228 0.023 518 0.000 407 433 166 196 10 150 3 3 1 047 3 364 0.3 0.050 216 0.001 491 0.178 715 0.005 492 0.025 583 0.000 314 206 36 167 5 163 2 4 881 2 141 0.4 0.106 611 0.005 091 0.370 730 0.018 204 0.024 900 0.000 282 1 743 87 320 13 159 2 5 1 181 2 404 0.5 0.212 831 0.011 149 0.921 408 0.058 786 0.029 593 0.000 674 2 927 85 663 31 188 4 6 1 195 3 125 0.4 0.155 669 0.007 417 0.681 328 0.039 838 0.029 793 0.000 588 2 409 81 528 24 189 4 7 978 2 675 0.4 0.048 219 0.001 730 0.164 494 0.005 876 0.024 751 0.000 336 109 79 155 5 158 2 8 854 4 196 0.2 0.050 422 0.001 721 0.167 094 0.005 727 0.023 981 0.000 271 213 50 157 5 153 2 9 1 466 3 968 0.4 0.067 995 0.002 499 0.240 261 0.009 048 0.025 520 0.000 321 878 76 219 7 162 2 10 920 2 634 0.3 0.054 946 0.002 215 0.197 121 0.008 193 0.025 945 0.000 372 409 91 183 7 165 2 11 1 450 2 688 0.5 0.066 240 0.002 423 0.223 225 0.008 345 0.024 427 0.000 317 813 72 205 7 156 2 12 450 1 479 0.3 0.093 773 0.005 922 0.350 126 0.025 724 0.025 564 0.000 422 1 503 115 305 19 163 3 13 1 556 7 569 0.2 0.081 278 0.002 663 0.282 509 0.009 287 0.025 136 0.000 250 1 228 69 253 7 160 2 14 199 299 0.7 0.055 158 0.004 664 0.242 086 0.017 684 0.029 846 0.000 537 420 191 220 14 190 3 15 277 448 0.6 0.051 077 0.003 054 0.169 254 0.009 829 0.023 300 0.000 408 243 137 159 9 148 3 16 860 1 847 0.5 0.052 317 0.001 823 0.184 399 0.006 440 0.025 627 0.000 352 298 80 172 6 163 2 17 841 2 369 0.4 0.051 139 0.001 884 0.174 810 0.006 277 0.024 793 0.000 267 256 82 164 5 158 2 18 1 181 2 894 0.4 0.053 895 0.001 849 0.191 353 0.006 436 0.025 740 0.000 300 365 78 178 5 164 2 19 1 976 4 897 0.4 0.058 698 0.002 288 0.210 398 0.008 430 0.025 805 0.000 298 567 81 194 7 164 2 20 2 180 5 476 0.4 0.058 450 0.002 297 0.192 465 0.007 516 0.023 807 0.000 337 546 87 179 6 152 2 
下载: 导出CSV
-
Bai, D. Y., Jia, B. H., Zhong, X., et al., 2012. Study on the Deformation of Indosinian Movement in Southeastern Hunan. Geological Review, 58(1): 19-29 (in Chinese with English abstract). Cawood, P. A., Hawkesworth, C. J., Dhuime, B., 2012. Detrital Zircon Record and Tectonic Setting. Geology, 40(10): 875-878. https://doi.org/10.1130/g32945.1 Chen, A., 1999. Mirror-Image Thrusting in the South China Orogenic Belt: Tectonic Evidence from Western Fujian, Southeastern China. Tectonophysics, 305(4): 497-519. https://doi.org/10.1016/S0040-1951(99)00036-0 Di, W., Li, R., Chen, J. F., et al., 2017. LA-ICP-MS Zircon U-Pb Age, Geochemistry and the Geological Significance of the Dapu Granite, Guangdong Province. Geological Science and Technology Information, 36(6): 148-157 (in Chinese with English abstract). Gan, C. S., Zhang, Y. Z., Wang, Y. J., et al., 2021. Reappraisal of the Mesozoic Tectonic Transition from the Paleo-Tethyan to Paleo-Pacific Domains in South China. Geological Society of America Bulletin, 133(11/12): 2582-2590. https://doi.org/10.1130/B35755.1 Guan, Y. X., Huang, Y. M., Tao, J. H., 1989. A Preliminary Discussion on Nappe Structure in Fujian. Geology of Fujian, 8(1): 14-34 (in Chinese with English abstract). Guangdong Provincial Bureau of Geology and Mineral Resources, 1988. Regional Geology of Guangdong Province. Geological Publishing House, Beijing (in Chinese). Guo, F., Fan, W. M., Li, C. W., et al., 2012. Multi-Stage Crust-Mantle Interaction in SE China: Temporal, Thermal and Compositional Constraints from the Mesozoic Felsic Volcanic Rocks in Eastern Guangdong-Fujian Provinces. Lithos, 150: 62-84. https://doi.org/10.1016/j.lithos.2011.12.009 Hu, S. M., Shan, Y. H., Zheng, J., 2021. Characteristics and Implication of Polyphase Folds in Upper Paleozoic Strata, South of Ansha Reservoir, Southwestern Fujian Province. Geotectonica et Metallogenia, 45(2): 255-269 (in Chinese with English abstract). Hu, S. M., Shan, Y. H., Zheng, J., et al., 2023. Characteristics of Middle-Late Triassic Structural Deformation in Central Southwestern Fujian. Geotectonica et Metallogenia, 47(3): 506-522 (in Chinese with English abstract). Hunan Provincial Bureau of Geology and Mineral Resources, 1988. Regional Geology of Hunan Province. Geological Publishing House, Beijing (in Chinese). Li, C. L., Wang, Z. X., Tan, Y. L., et al., 2023. Differential Fold Interference Patterns in an Intracontinental Orogen: Insights from Superposed Buckle Folding in Southern Jiangxi Province, South China Block. Journal of Structural Geology, 167: 104801. https://doi.org/10.1016/j.jsg.2023.104801 Li, J. H., Cawood, P. A., Ratschbacher, L., et al., 2020. Building Southeast China in the Late Mesozoic: Insights from Alternating Episodes of Shortening and Extension along the Lianhuashan Fault Zone. Earth-Science Reviews, 201: 103056. https://doi.org/10.1016/j.earscirev.2019.103056 Li, J. H., Dong, S. W., Cawood, P. A., et al., 2018. An Andean-Type Retro-Arc Foreland System beneath Northwest South China Revealed by Sinoprobe Profiling. Earth and Planetary Science Letters, 490: 170-179. https://doi.org/10.1016/j.epsl.2018.03.008 Li, J. H., Dong, S. W., Zhao, G. C., et al., 2024. Late Mesozoic Continental Deformation, Deep Processes, and Geodynamic Evolution of South China. Acta Geologica Sinica, 98(3): 829-861 (in Chinese with English abstract). Li, J. H., Zhang, Y. Q., Dong, S. W., et al., 2012. Late Mesozoic-Early Cenozoic Deformation History of the Yuanma Basin, Central South China. Tectonophysics, 570: 163-183. https://doi.org/10.1016/j.tecto.2012.08.012 Li, R., Wang, J. R., Ling, K., et al., 2021. Division of Mesozoic Volcanic Cycles in the Fengshun Area, Eastern Guangdong Province. South China Geology, 37(1): 29-44 (in Chinese with English abstract). Li, Z. X., Li, X. H., 2007. Formation of the 1 300-km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China: A Flat-Slab Subduction Model. Geology, 35(2): 179. https://doi.org/10.1130/g23193a.1 Liu, Y. S., Gao, S., Hu, Z. C., et al., 2010a. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths. Journal of Petrology, 51(1-2): 537-571. https://doi.org/10.1093/petrology/egp082 Liu, Y. S., Hu, Z. C., Zong, K. Q., et al., 2010b. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15): 1535-1546. https://doi.org/10.1007/s11434-010-3052-4 Qiu, Y. X., Qiu, J. S., Li, J. C., et al., 1991. Deformational and Metamorphic Features of Lianhuashan Fault Zone during Meso-Cenozoic Time and Mechanism of Their Formation. Journal of Geomechanics, (14): 93-106 (in Chinese with English abstract). Shang, L. N., Pan, J., Cao, R., et al., 2024. Structural Characteristics of the Binhai Fault Zone in Jiangsu Offshore—Implications from Gravity and Magnetic Data. East China Geology, 45(1): 101-114 (in Chinese with English abstract). Shi, W., Dong, S. W., Zhang, Y. Q., et al., 2015. The Typical Large-Scale Superposed Folds in the Central South China: Implications for Mesozoic Intracontinental Deformation of the South China Block. Tectonophysics, 664: 50-66. https://doi.org/10.1016/j.tecto.2015.08.039 Shu, L. S., Zhou, X. M., Deng, P., et al., 2009. Mesozoic Tectonic Evolution of the Southeast China Block: New Insights from Basin Analysis. Journal of Asian Earth Sciences, 34(3): 376-391. https://doi.org/10.1016/j.jseaes.2008.06.004 Wang, D. Y., Li, M. X., Wang, Q., et al., 2024. Magmatic Response to Lithospheric Thinning of the North China Craton—Evidence from the Daqingshan Granite. East China Geology, 45(2): 173-186 (in Chinese with English abstract). Wang, W. F., Wang, Q., Shan, X. J., 2018. Development Characteristics and Formation Mechanism of Transverse Faults along the Kuqa Thrust Belt. Geology in China, 45(3): 493-510 (in Chinese with English abstract). Wang, Y. J., Fan, W. M., Zhang, G. W., et al., 2013. Phanerozoic Tectonics of the South China Block: Key Observations and Controversies. Gondwana Research, 23(4): 1273-1305. https://doi.org/10.1016/j.gr.2012.02.019 Wang, Y. J., Wang, Y., Zhang, Y. Z., et al., 2021. Triassic Two-Stage Intra-Continental Orogensis of the South China Block, Driven by Paleotethyan Closure and Interactions with Adjoining Blocks. Journal of Asian Earth Sciences, 206: 104648. https://doi.org/10.1016/j.jseaes.2020.104648 Xin, Y. J., Li, J. H., Zhang, Y. Q., et al., 2023. Episodic Magmatism in the Lianhuashan Tectonic Belt: Implications for Late Mesozoic Crustal Reworking in SE South China. GSA Bulletin, 135(11-12): 3043-3065. https://doi.org/10.1130/b36504.1 Xu, Q. J., Liu, S. F., Wang, Z. F., et al., 2019. Provenance of the East Guangdong Basin and Yong'an Basin in Southeast China: Response to the Mesozoic Tectonic Regime Transformation. Journal of Asian Earth Sciences, 185: 104024. https://doi.org/10.1016/j.jseaes.2019.104024 Xu, X. B., 2023. Late Triassic to Middle Jurassic Tectonic Evolution of the South China Block: Geodynamic Transition from the Paleo-Tethys to the Paleo-Pacific Regimes. Earth-Science Reviews, 241: 104404. https://doi.org/10.1016/j.earscirev.2023.104404 Xu, X. B., Liang, C. H., Xu, Y. D., 2021. Kinematic Analysis of Fault-Slip Data in the Nanling Tectonic Belt and Cretaceous to Paleogene Tectonic Evolution of the Central South China Block. Journal of Asian Earth Sciences, 221: 104951. https://doi.org/10.1016/j.jseaes.2021.104951 Xu, X. B., Tang, S., Lin, S. F., 2016. Paleostress Inversion of Fault-Slip Data from the Jurassic to Cretaceous Huangshan Basin and Implications for the Tectonic Evolution of Southeastern China. Journal of Geodynamics, 98: 31-52. https://doi.org/10.1016/j.jog.2016.03.013 Xu, X. B., Zhang, Y. Q., Jia, D., et al., 2009. Early Mesozoic Geotectonic Processes in South China. Geology in China, 36(3): 573-593 (in Chinese with English abstract). Xu, X. B., Zhang, Y. Q., Jia, D., et al., 2010. Geochronology of Zircon LA-ICP-MS U-Pb and Muscovite 40Ar/39Ar: Constrains to Early Yanshanian Event in Southeast China. Geological Science and Technology Information, 29(2): 87-94 (in Chinese with English abstract). Xu, X. B., Zhang, Y. Q., Jia, D., et al., 2011. U-Pb Dating of Volcanic Rocks and Granites along the Wuyishan Belt: Constraints on Tuning of Late Mesozoic Tectonic Events in Southeast China. Acta Geologica Sinica, 85(1): 130-144. https://doi.org/10.1111/j.1755-6724.2011.00385.x Zhang, X. C., Wang, Y. J., Harris, R., et al., 2019. Discovery of Middle-Late Devonian and Early Permian Magmatic Events in East Asia and Their Implication for the Indosinian Orogeny in South China: Insights from the Sedimentary Record. GSA Bulletin, 131(9/10): 1519-1536. https://doi.org/10.1130/b35032.1 Zhang, Y. Q., Dong, S. W., Li, J. H., et al., 2012. The New Progress in the Study of Mesozoic Tectonics of South China. Acta Geoscientica Sinica, 33(3): 257-279 (in Chinese with English abstract). Zhang, Y. Q., Xu, X. B., Jia, D., et al., 2009. Deformation Record of the Change from Indosinian Collision-Related Tectonic System to Yanshanian Subduction-Related Tectonic System in South China during the Early Mesozoic. Earth Science Frontiers, 16(1): 234-247 (in Chinese with English abstract). Zhou, X. M., Li, W. X., 2000. Origin of Late Mesozoic Igneous Rocks in Southeastern China: Implications for Lithosphere Subduction and Underplating of Mafic Magmas. Tectonophysics, 326(3/4): 269-287. https://doi.org/10.1016/S0040-1951(00)00120-7 Zhuo, W. H., Zhang, Z. J., Wu, X. H., et al., 2011. New Progresses in 1: 50 000 Regional Geological Survey in Meizhou Area, Eastern Guangdong Province. Geology and Mineral Resources of South China, 27(4): 319-326(in Chinese with English abstract). Zou, H. P., Wang, J. H., Qiu, Y. X., 2000. 40Ar/39Ar Ages of the Nan'ao Shear Zone and the Lianhuashan Shear Zone in Guangdong Province and Their Geological Significance. Acta Geoscientica Sinica, 21(4): 356-364 (in Chinese with English abstract). 柏道远, 贾宝华, 钟响, 等, 2012. 湘东南印支运动变形特征研究. 地质论评, 58(1): 19-29. 邸文, 李瑞, 陈俊锋, 等, 2017. 广东大埔岩体LA-ICP-MS锆石U-Pb年龄、地球化学及其地质意义. 地质科技情报, 36(6): 148-157. 关玉祥, 黄耀明, 陶建华, 1989. 初论福建推覆构造. 福建地质, 8(1): 14-34. 广东省地质矿产局, 1988. 广东省区域地质志. 北京: 地质出版社. 胡斯敏, 单业华, 郑剑, 2021. 闽西南安砂水库南岸上古生界的多期褶皱特征及其意义. 大地构造与成矿学, 45(2): 255-269. 胡斯敏, 单业华, 郑剑, 等, 2023. 闽西南坳陷中部中-晚三叠世构造变形特征. 大地构造与成矿学, 47(3): 506-522. 湖南省地质矿产局, 1988. 湖南省区域地质志. 北京: 地质出版社. 李建华, 董树文, 赵国春, 等, 2024. 华南晚中生代大陆变形、深部过程及动力学. 地质学报, 98(3): 829-861. 李瑞, 王建荣, 凌恳, 等, 2021. 粤东丰顺地区中生代火山活动旋回划分. 华南地质, 37(1): 29-44. 邱元禧, 邱津松, 李建超, 等, 1991. 广东莲花山断裂带中、新生代多期复合变形变质带的基本特征及其形成机制的探讨. 中国地质科学院地质力学研究所所刊, (14): 93-106. 尚鲁宁, 潘军, 曹瑞, 等, 2024. 基于重磁数据研究江苏岸外滨海断裂带及邻区构造特征. 华东地质, 45(1): 101-114. 王丹阳, 李猛兴, 王权, 等, 2024. 华北克拉通减薄的岩浆浅表响应: 来自大青山岩体的证据. 华东地质, 45(2): 173-186. 王伟锋, 王乾, 单新建, 2018. 库车前陆冲断带横断层发育特征及其形成机制. 中国地质, 45(3): 493-510. 徐先兵, 张岳桥, 贾东, 等, 2009. 华南早中生代大地构造过程. 中国地质, 36(3): 573-593. 徐先兵, 张岳桥, 贾东, 等, 2010. 锆石La-ICP-MS U-Pb与白云母40Ar/39Ar年代学及其对中国东南部早燕山事件的制约. 地质科技情报, 29(2): 87-94. 张岳桥, 董树文, 李建华, 等, 2012. 华南中生代大地构造研究新进展. 地球学报, 33(3): 257-279. 张岳桥, 徐先兵, 贾东, 等, 2009. 华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录. 地学前缘, 16(1): 234-247. 卓伟华, 张忠进, 吴小辉, 等, 2011. 粤东梅州地区1∶5万区调主要成果与进展. 华南地质与矿产, 27(4): 319-326. 邹和平, 王建华, 丘元禧, 2000. 广东南澳和莲花山韧性剪切带40Ar/39Ar年龄及其地质意义. 地球学报, 21(4): 356-364. -
点击查看大图
图(9) / 表(1)
计量
- 文章访问数: 40
- HTML全文浏览量: 15
- PDF下载量: 10
- 被引次数: 0
