Paleoproterozoic Back-Arc Basin Opening and Closure: Evidence from the Structural Research of the Volcanic-Sedimentary Rocks in the Helan Town, Liaodong Peninsula
-
摘要: 前寒武纪盆地演化及造山作用一直是造山带研究中的热点和难点，通过对华北克拉通东部陆块胶-辽-吉构造带中辽东半岛河栏镇火山-沉积岩进行深入的野外及室内研究，反演该地区古元古代大地构造演化过程.通过对辽河群里尔峪组火山岩、高家峪组钙质泥岩以及大石桥组碳酸盐岩野外的详细构造解析，识别出各类岩石单元中发育同沉积伸展构造（D1-0），包括同沉积不对称褶皱、层间平卧褶皱和滑脱面理及线理，指示辽吉弧后盆地早期伸展张裂过程.通过对河栏镇蒲石河地区基性侵入岩及喷出枕状熔岩进行详细的野外构造填图及解析，提出伴随基性枕状熔岩的喷发，辽吉弧后盆地张裂到最大程度.此外，在各组相关岩石中观察到大量逆冲推覆构造及不对称断展褶皱，构造归为D1-1或者D1-2，指示辽吉弧后盆地受挤压应力影响发生收缩.锆石年代学研究指示高家峪组沉积物物源主要来自于~2.5 Ga基底，少量来自古元古代（2 172 Ma）火山弧.综合区域内已有岩石地球化学及年代学资料，研究表明辽吉弧后盆地的拉张及闭合过程伴随着古元古代增生造山作用，并暗示板块构造在古元古代已经开启.Abstract: Precambrian orogenesis has always been a hot and challenging issue in the study of accretionary and collisional orogenic belts. In this paper, we study the volcanic-sedimentary rocks in the Paleoproterozoic Jiao-Liao-Ji orogenic belt at the Helan Town in the Liaodong Peninsula using methods of detailed mapping in the field and age dating indoors, and finally decipher the Paleoproterozoic evolution of this area in the eastern China Block of the North China Craton. Many syn-depositional structures such as asymmetric folds, isoclinal folds, and inter-bedding slip lineations were recognized and classified as syn-depositional structures based on our detailed field structural analysis of the volcanic rocks from the Li'eryu Formation, calcareous mudstones from the Gaojiayu Formation, and carbonates from the Dashiqiao Formation. We further classified these structures as D1-0, which formed in an extensional process at the early opening stage of the Liaoji back-arc basin. Based on detailed field mapping of the intrusive mafic rocks and its related eruption "pillow lava" in the Pushihe area of Helan Town, it was proposed that the eruption of the basic "pillow lava" indicates that the Liaoji back-arc basin turned into the maximum extension stage. Besides, a large number of thrust nappe structures and asymmetric fault-propagation folds were observed in the volcanic rocks of the Li'eryu Formation, the calcareous mudstones of the Gaojiayu Formation, and the carbonates of the Dashiqiao Formation in the Liaohe Group, and were defined as D1-1 or D1-2. These structures indicate the contraction of the Liaoji back-arc basin, also imply the beginning of the Paleoproterozoic orogenesis. Detrital zircon study of the Gaojiayu Formation indicates that the predominated provenance of the clastics was from a 2.5 Ga basement, and few of them were from the 2.17 Ga volcanic rocks. Combined with petro-geochemistry and geochronology data in our study area, it is concluded that the opening and closure of the Liaoji back-arc basin recorded a complete Paleoproterozoic orogenesis process and also indicated the plate tectonic initiation at the time.
-
图 1 华北克拉通大地构造划分区图(修改自Zhao et al., 2005)
Fig. 1. Tectonic subdivision of the North China Craton (modified after Zhao et al., 2005)
图 2 辽东半岛河栏镇地区地质图
图修改自辽宁省第一区域地质测量队二分队(1971)完成的中华人民共和国地质图 1:20万辽阳幅K-51-XXVII；剖面A-A’、B-B’、C-C’、D-D’和E-E’的位置标注于此图上.高家峪剖面(图 5a)也标注于此图上
Fig. 2. Simplified geological map of the Helan Town region, Liaodong Penisula
图 3 北辽河群柱状图
图中年代学数据引自Wang et al.(2016)和Xu et al.(2020)
Fig. 3. Simplified geological column map of the North Liaohe Group
图 4 辽东半岛河栏镇地区里尔峪组火山岩野外照片及构造变形特征
a.流纹岩野外特征，S0流动面理发育，气孔状构造发育；b.火山角砾岩发育；c.流纹岩镜下特征，气孔中填充方解石；d.同岩浆构造，指示火山岩左行向下的伸展性流动特征；e.角砾岩滑塌堆积；f.含黄铁矿火山岩；g.含黄铁矿火山岩镜下照片，黄铁矿沿S0面理沉积，指示其喷流沉积特征；h~i.火山沉积岩S0面理发生变形，倒转褶皱发育，褶皱轴面倾向南(见右侧极射赤平投影图)，寄生褶皱发育
Fig. 4. Field photos and structural deformation characteristics of volcanic rocks in the Li'eryu Formation in the Helan Town, Liaodong Peninsula
图 5 辽东半岛河栏镇地区高家峪组野外照片及构造变形特征
a.河栏镇北高家峪组典型剖面；b.泥晶灰岩中斜层理发育；c.泥晶灰岩中钙质泥岩夹层，Z字形不对称褶皱发育，指示同沉积伸展性构造特征；d.泥晶灰岩中钙质泥岩夹层发育层间平卧褶皱；e~f.高家峪组受后期逆冲推覆构造改造，发育典型的双冲构造duplex，其几何学特征指示由南向北的运动学特征；g~h.地层受到后期断层及断层相关褶皱改造，断展褶皱发育明显，不对称褶皱轴面几何学特征指示由南向北的运动学特征
Fig. 5. Field photos and structural deformation characteristics of the Gaojiayu Formation in the Helan Town, Liaodong Peninsula
图 6 辽东半岛河栏镇地区高家峪组碎屑锆石阴极发光图像、频率分布直方图、谐和图(谐和度≥90%)，
a、c和d.样品17TZH10-1来自剖面偏底部钙质砂泥岩；b、e和f.样品17TZH18-1来自剖面偏上部的钙质泥岩
Fig. 6. Representative cathodoluminescence (CL) images, probability density plot, concordia diagram (concordance ≥90%) of the Gaojiayu Formation at the northern part of Helan Town, Liaodong Peninsula
图 7 早期辉绿岩侵入大理岩中，将大理岩顶起呈穹窿状特征，其中辉绿岩侵入面上可见流动性线理，大理岩与辉绿岩侵入体接触面局部较为温和，局部呈切层侵入状(a)；露头上可见辉绿岩岩浆上涌过程中吞噬大理岩的过程，可见大理岩捕虏体于辉绿岩中(b)
Fig. 7. Diabase intruded into the marbles, the marble shows dome-like feature because of intrusion, flow foliation can be observed on the surface of diabase. Between the marble and diabase, some local areas show gentle contact, some local areas show bedding crosscut contact (a); outcrop shows marble xenolith in diabase because of the mafic magma upwelling and intrusion (b)
图 8 辉绿岩侵入碳酸盐岩后，大理岩从A到C出现原生面理S0及平行S0面理S0-1产状变缓趋势，面理上早期的拉伸线理L0-1也趋于变缓，极射赤平投影图显示其变化产状特征(a)；大理岩中背斜(c和d)；碳酸盐岩中逆冲推覆构造发育，显示双冲构造特征(b)
Fig. 8. After intrusion of diabase, the dipping angle of original S0 and S0 parallel foliation S0-1 are getting lower from A to C, lineations L0-1 on S0-1 surface also show this feature, data are presented in the projection (a), fold in marble (c and d), duplexes developed in the marbles (b)
图 9 辽东半岛河栏镇蒲石河地区枕状熔岩野外大比例尺填图及野外照片
可见填图区枕状熔岩发育较为连续的区域(①)和发育不连续区域(②)
Fig. 9. Pillow lava developed in the Helan Town, Liaodong Peninsula, detail large scale geological mapping was carried out in the Pushihe area
图 10 辽东半岛河栏镇地区五条典型构造剖面
剖面A-A’显示太古宙基底到高家峪组及构造，修改自Tian et al.(2020)；剖面B-B’显示河栏镇地区里尔峪组与高家峪组之间关系；剖面C-C’显示河栏镇地区基性侵入岩与碳酸盐岩(大理岩)之间关系；剖面D-D’展示大理岩变形特征，修改自Tian et al.(2017)；剖面E-E’显示盖县组片岩变形特征及其辽河群与辽吉花岗岩之间的关系，修改自Tian et al.(2017)
Fig. 10. Five typical cross-sections developed in the Helan Town, Liaodong Peninsula
图 11 辽东半岛河栏镇蒲石河地区枕状熔岩形成过程示意
a.辽吉弧后盆地张裂至最大，大量基性岩浆上涌；b.岩浆部分侵入碳酸盐岩中，部分在海底冷却；c.基性岩形成大量节理，给流体提供通道，形成水下枕状熔岩雏形；d.后期造山作用改造，形成现今枕状熔岩形态.
Fig. 11. Cartoon maps show the formation of Pushihe pillow lava in the Helan Town, Liaodong Peninsula
图 12 辽东半岛辽吉弧后盆地大地构造演化过程
a.古元古代2 200~2 170 Ma，龙岗基底南侧呈被动大陆边缘特征；b. 2 170 Ma，被动大陆边缘转换为活动大陆边缘；c. 2 170~2 115 Ma，辽吉弧后盆地持续张裂，枕状熔岩出现指示盆地张裂至最大程度；d.~1 950 Ma，辽吉地区进入最强造山作用时期.
Fig. 12. Tectonic evolution of the Liaoji back-arc basin, Liaodong Peninsula
表 1 辽河群各组岩石单元变质-变形特征及其变形时代
Table 1. Metamorphic-deformational feature of each formation in the Liaohe Group and its related deformational age
浪子山组 里尔峪组 高家峪组 大石桥组 盖县组 变形时代 岩性 石英岩含蓝晶石-十字石-石榴子石片岩、千枚岩 火山岩大理岩 板岩、钙质泥岩、碎屑灰岩、钙质砂岩 结晶灰岩、大理岩 片岩、变质粉砂岩 变形 D1-0 无痕迹 同沉积、同岩浆不对称褶皱 同沉积不对称褶皱、平卧褶皱、同斜褶皱 同沉积断层发育、滑脱型面理及线理 局部可见S0 2 200~ 2 115 Ma* D1-1 局部见F1、S1、L1 F1、S1发育 F1、S1发育、逆冲断层 F1、S1发育 S1、L1 2 115~ 1 950 Ma** D1-2 褶劈理S2发育、逆冲推覆构造发育，倒转褶皱F2发育, 倒转褶皱F2发育 直立褶皱F2发育 F2发育 S2发育、L2局部可见 1 950 Ma** D1-3 膝折发育 未见 未见 F3局部发育 1 950~ 1 840 Ma*** 变质 角闪岩相 整体较低 整体较低，局部未变质 整体较低，局部未变质 局部变质 侵入岩 见少量基性岩侵入 见少量基性岩侵入 见少量基性岩侵入 见大量基性岩侵入，枕状熔岩 未见基性侵入岩 注：*据 Wang et al.(2016) ；**据Liu et al.(2019) ；***据Tian et al.(2017) .
下载: 导出CSV
-
Bai, J., 1993. The Precambrian Geology and Pb⁃Zn Mineralization in the Northern Margin of North China Platform. Geological Publishing House, Beijing (in Chinese with English abstract). Bi, J. H., Ge, W. C., Xing, D. H., et al., 2018. Palaeoproterozoic Meta⁃Rhyolite and Meta⁃Dacite of the Liaohe Group, Jiao⁃Liao⁃Ji Belt, North China Craton: Petrogenesis and Implications for Tectonic Setting. Precambrian Research, 314: 306-324. https://doi.org/10.1016/j.precamres.2018.06.007" target="_blank"> https://doi.org/10.1016/j.precamres.2018.06.007 Cai, J., Liu, F. L., Liu, P. H., et al., 2020. Metamorphic P-T Evolution and Tectonic Implications of Pelitic Granulites in the Ji'an Area, Northeastern Jiao–Liao–Ji Belt, North China Craton. Journal of Asian Earth Sciences, 191: 104197. https://doi.org/10.1016/j.jseaes.2019.104197" target="_blank"> https://doi.org/10.1016/j.jseaes.2019.104197 Chen, J. S., Xing, D. H., Liu, M., et al., 2017. Zircon U–Pb Chronology and Geological Significance of Felsic Volcanic Rocks in the Liaohe Group from the Liaoyang Area, Liaoning Province. Acta Petrologica Sinica, 33(9): 2792-2810 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201709010.htm Dong, C. Y., Wan, Y. S., Xie, H. Q., et al., 2017. The Mesoarchean Tiejiashan⁃Gongchangling Potassic Granite in the Anshan⁃Benxi Area, North China Craton: Origin by Recycling of Paleo⁃ to Eoarchean Crust from U⁃Pb⁃Nd⁃Hf⁃O Isotopic Studies. Lithos, 290-291: 116-135. https://doi.org/10.1016/j.lithos.2017.08.009" target="_blank"> https://doi.org/10.1016/j.lithos.2017.08.009 Faure, M., Lin, W., Monié, P., et al., 2004. Palaeoproterozoic Arc Magmatism and Collision in Liaodong Peninsula (North⁃East China). Terra Nova, 16(2): 75-80. https://doi.org/10.1111/j.1365⁃3121.2004.00533.x doi: 10.1111/j.1365⁃3121.2004.00533.x Han, C. M., Xiao, W. J., Su, B. X., et al., 2014. Formation Age and Genesis of the Gongchangling Neoarchean Banded Iron Deposit in Eastern Liaoning Province: Constraints from Geochemistry and SHRIMP Zircon U–Pb Dating. Precambrian Research, 254: 306-322. https://doi.org/10.1016/j.precamres.2014.09.007" target="_blank"> https://doi.org/10.1016/j.precamres.2014.09.007 He, G. P., Ye, H. W., 1998. Compostion and Mian Characteristics of Early Proterozoic Metamorphic Terranes in Eastern Liaoning and Southern Jilin Areas. Journal of Changchuang University of Science and Techology, 28(2): 121-134 (in Chinese with English abstract). http://www.researchgate.net/publication/302879243_Compositions_and_main_characteristics_of_Early_Proterozoic_metamorphic_terrains_in_the_eastern_Liaoning_and_the_southern_Jilin_areas Li, S. Z., Zhao, G. C., Sun, M., et al., 2005. Deformation History of the Paleoproterozoic Liaohe Assemblage in the Eastern Block of the North China Craton. Journal of Asian Earth Sciences, 24(5): 659-674. https://doi.org/10.1016/j.jseaes.2003.11.008" target="_blank"> https://doi.org/10.1016/j.jseaes.2003.11.008 Li, X. Y., Zhang, L. H., 1990. Geochemical Features of Some Major Metamorphoc Rocks in Liaohe Group. Land & Resources, (3): 199-211 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-LOAD199003001.htm Li, Z., Chen, B., 2014. Geochronology and Geochemistry of the Paleoproterozoic Meta⁃Basalts from the Jiao⁃Liao⁃Ji Belt, North China Craton: Implications for Petrogenesis and Tectonic Setting. Precambrian Research, 255: 653-667. https://doi.org/10.1016/j.precamres.2014.07.003" target="_blank"> https://doi.org/10.1016/j.precamres.2014.07.003 Liu, F. L., Liu, C. H., Itano, K., et al., 2017a. Geochemistry, U⁃Pb Dating, and Lu⁃Hf Isotopes of Zircon and Monazite of Porphyritic Granites within the Jiao⁃Liao⁃Ji Orogenic Belt: Implications for Petrogenesis and Tectonic Setting. Precambrian Research, 300: 78-106. https://doi.org/10.1016/j.precamres.2017.08.007" target="_blank"> https://doi.org/10.1016/j.precamres.2017.08.007 Liu, F. L., Liu, P. H., Wang, F., et al., 2015. Progresses and Overviews of Voluminous Meta⁃Sedimentary Series within the Paleoproterozoic Jiao⁃Liao⁃Ji Orogenic. Acta Petrologica Sinica, 31(10): 2816-2846 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201510002.htm Liu, P. H., Cai, J., Zou, L., 2017a. Metamorphic P⁃T⁃t Path and Its Geological Implication of the Sanjiazi Garnet Amphibolites from the Northern Liaodong Penisula, Jiao⁃Liao⁃Ji Belt: Constraints on Phase Equilibria and Zircon U⁃Pb Dating. Acta Petrologica Sinica, 33(9): 2649-2674 (in Chinese with English abstract). Liu, P. H., Liu, F. L., Cai, J., et al., 2017b. Discovery and Geological Significance of High⁃Pressure Mafic Granulites in the Pingdu⁃Anqiu Area of the Jiaobei Terrane, the Jiao⁃Liao⁃Ji Belt, the North China Craton. Precambrian Research, 303: 445-469. https://doi.org/10.1016/j.precamres.2017.05.022" target="_blank"> https://doi.org/10.1016/j.precamres.2017.05.022 Liu, P. H., Liu, F. L., Tian, Z. H., et al., 2017b. Barrovian⁃Type Metamorphism and Deformation Histroy of the North Liaohe Grup in the Liaoyang⁃Benxi Area, Liaodong Penenisula, Implication for the Paleoproterozoic Orogenesis in the Jiao⁃Liao⁃Ji Orogenic Belt. 2017 CGU, Beijing (in Chinese). Liu, P. H., Liu, F. L., Tian, Z. H., et al., 2019. Petrological and Geochronological Evidence for Paleoproterozoic Granulite⁃Facies Metamorphism of the South Liaohe Group in the Jiao⁃Liao⁃Ji Belt, North China Craton. Precambrian Research, 327: 121-143. https://doi.org/10.1016/j.precamres.2019.03.002" target="_blank"> https://doi.org/10.1016/j.precamres.2019.03.002 Liu, Y. D., Bing, Z. H., Dong, J. C., 1989. Features of the Early Proetrozoic Pilow Lava in Liaodong Peninsula. Liaoning Geology, (4): 206-215 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-LOAD198903001.htm Liu, Y. J., Yang, Z. S., Li, S. Z., et al., 1997. Extensional Tectonic Model of Palaeoproterozoic: An Example from Northern Shangdong Peninsula, Eastern Liaoning and Southern Jilin Areas. Journal of Changchun University of Earth Sciences, 27(2): 141-146 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ702.003.htm Liu, Y. S., Gao, S., Hu, Z. C., et al., 2010. 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" target="_blank"> https://doi.org/10.1093/petrology/egp082 Lu, L. Z., Xiu, X. C., Liu, F. L., 1996. Early Precambrian Khondalite Series in North China. Changchun Publishing House, Changchun, 195-234 (in Chinese). Lu, X. P., Wu, F. Y., Guo, J. H., et al., 2006. Zircon U–Pb Geochronological Constraints on the Paleoproterozoic Crustal Evolution of the Eastern Block in the North China Craton. Precambrian Research, 146(3-4): 138-164. https://doi.org/10.1016/j.precamres.2006.01.009" target="_blank"> https://doi.org/10.1016/j.precamres.2006.01.009 Ludwig, K., 2003. User's Manual for Isoplot 3.6: a Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Berkeley. Luo, Y., Sun, M., Zhao, G. C., et al., 2004. LA⁃ICP⁃MS U–Pb Zircon Ages of the Liaohe Group in the Eastern Block of the North China Craton: Constraints on the Evolution of the Jiao⁃Liao⁃Ji Belt. Precambrian Research, 134(3-4): 349-371. https://doi.org/10.1016/j.precamres.2004.07.002" target="_blank"> https://doi.org/10.1016/j.precamres.2004.07.002 Meng, E., Liu, F. L., Liu, P. H., et al., 2014. Petrogenesis and Tectonic Significance of Paleoproterozoic Meta⁃Mafic Rocks from Central Liaodong Peninsula, Northeast China: Evidence from Zircon U–Pb Dating and in Situ Lu–Hf Isotopes, and Whole⁃Rock Geochemistry. Precambrian Research, 247: 92-109. https://doi.org/10.1016/j.precamres.2014.03.017" target="_blank"> https://doi.org/10.1016/j.precamres.2014.03.017 Tam, P. Y., Zhao, G. C., Liu, F. L., et al., 2011. Timing of Metamorphism in the Paleoproterozoic Jiao⁃Liao⁃Ji Belt: New SHRIMP U–Pb Zircon Dating of Granulites, Gneisses and Marbles of the Jiaobei Massif in the North China Craton. Gondwana Research, 19(1): 150-162. https://doi.org/10.1016/j.gr.2010.05.007" target="_blank"> https://doi.org/10.1016/j.gr.2010.05.007 Tang, H. S., Chen, Y. J., Wu, G., et al., 2008. The C⁃O Isotope Composition of the Liaohe Group, Northern Liaoning Province and Its Geologic Implications. Acta Petrologica Sinica, 24(1): 129-138. http://www.oalib.com/paper/1472736 Tian, Z. H., Liu, F. L., Liu, P. H., et al., 2020. A Paleoproterozoic Nappe on Meso⁃Archean Gneisses Exhumed by a Cretaceous Metamorphic Core Complex in Northeastern North China Craton. International Journal of Earth Sciences, 109: 1403-1420. https://doi.org/10.1007/s00531⁃020⁃01870⁃4 doi: 10.1007/s00531⁃020⁃01870⁃4 Tian, Z. H., Liu, F. L., Windley, B. F., et al., 2017. Polyphase Structural Deformation of Low⁃ to Medium⁃Grade Metamorphic Rocks of the Liaohe Group in the Jiao⁃Liao⁃Ji Orogenic Belt, North China Craton: Correlations with Tectonic Evolution. Precambrian Research, 303: 641-659. https://doi.org/10.1016/j.precamres.2017.08.017" target="_blank"> https://doi.org/10.1016/j.precamres.2017.08.017 Wang, F., Liu, F. L., Liu, P. H., et al., 2017. In Situ Zircon U⁃Pb Dating and Whole⁃Rock Geochemistry of Metasedimentary Rocks from South Liaohe Group, Jiao⁃Liao⁃Ji Orogenic Belt: Constraints on the Depositional and Metamorphic Ages, and Implications for Tectonic Setting. Precambrian Research, 303: 764-780. https://doi.org/10.1016/j.precamres.2017.10.002" target="_blank"> https://doi.org/10.1016/j.precamres.2017.10.002 Wang, X. P., Peng, P., Wang, C., et al., 2016. Petrogenesis of the 2 115 Ma Haicheng Mafic Sills from the Eastern North China Craton: Implications for an Intra⁃Continental Rifting. Gondwana Research, 39: 347-364. https://doi.org/10.1016/j.gr.2016.01.009" target="_blank"> https://doi.org/10.1016/j.gr.2016.01.009 Wen, F., Tian, Z. H., Liu, P. H., et al., 2020. A Case Study of Barrovian Metamorphic Zone of Langzishan Formation of Northern Liaohe Group, Liaodong Peninsula. Earth Science, 45(9): 3403-3419 (in Chinese with English abstract). doi: 10.1007/s00531-020-01870-4 Xu, W., Liu, F. L., Liu, P. H., et al., 2020. Paleoproterozoic Transition in Tectonic Regime Recorded by the Eastern Block of the North China Craton: Evidence from Detrital Zircons of the Langzishan Formation, Jiao⁃Liao⁃Ji Belt. International Geology Review, 62(2): 168-185. https://doi.org/10.1080/00206814.2019.1594413" target="_blank"> https://doi.org/10.1080/00206814.2019.1594413 Xu, W., Liu, F. L., Tian, Z. H., et al., 2018. Source and Petrogenesis of Paleoproterozoic Meta⁃Mafic Rocks Intruding into the North Liaohe Group: Implications for Back⁃Arc Extension Prior to the Formation of the Jiao⁃Liao⁃Ji Belt, North China Craton. Precambrian Research, 307: 66-81. https://doi.org/10.1016/j.precamres.2018.01.011" target="_blank"> https://doi.org/10.1016/j.precamres.2018.01.011 Xu, W., Liu, F. L., Wang, F., et al., 2020. Palaeoproterozoic Tectonic Evolution of the Jiao–Liao–Ji Belt, North China Craton: Geochemical and Isotopic Evidence from Ca. 2.17 Ga Felsic Tuff. Geological Journal, 55(1): 409-424. https://doi.org/10.1002/gj.3380" target="_blank"> https://doi.org/10.1002/gj.3380 Yang, M. C., Chen, B., Yan, C., 2015. Petrogenesis of Paleoproterozoic Gneissic Granites from Jiao⁃Liao⁃Ji Belt of North China Craton and Their Tectonic Implications. Journal of Earth Sciences and Environment, 37(5): 31-51 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XAGX201505004.htm Yin, A., Brandl, G., Krö ner, A., 2020. Plate⁃Tectonic Processes at Ca. 2.0 Ga: Evidence from > 600 km of Plate Convergence. Geology, 48(2): 103-107. https://doi.org/10.1130/g47070.1" target="_blank"> https://doi.org/10.1130/g47070.1 Zhang, P., Zhao, Y., Kou, L. L., et al., 2019. Zircon U⁃Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaoning Peninsula. Earth Science, 44(10): 3297-3313 (in Chinese with English abstract). Zhang, Q. S., Yang, Z. S., 1988. Early Crust and Mineral Deposits of Liaodong Peninsula, China. Geological Publishing House, Beijing (in Chinese). Zhao, G. C., Sun, M., Wilde, S. A., et al., 2005. Late Archean to Paleoproterozoic Evolution of the North China Craton: Key Issues Revisited. Precambrian Research, 136(2): 177-202. https://doi.org/10.1016/j.precamres.2004.10.002" target="_blank"> https://doi.org/10.1016/j.precamres.2004.10.002 Zhao, Y., Kou, L. L., Zhang, P., et al., 2019. Characteristics of Geochemistry and Hf Isotope from Meta⁃Gabbro in Longchang Area, Liaodong Peninsula: Implications on Evolution of The Jiao⁃Liao⁃Ji Paleoproterozoic Orogenic Belt. Earth Science, 44(10): 3333-3345 (in Chinese with English abstract). Zhou, S. T., 1994. Geology Featre of the BIF in the Anshan⁃Benxi Area, Geological Publishing House, Beijing (in Chinese) Zhu, R. X., Zhang, H. F., Zhu, G., et al., 2017. Craton Destruction and Related Resources. International Journal of Earth Sciences, 106(7): 2233-2257. https://doi.org/10.1007/s00531⁃016⁃1441⁃x doi: 10.1007/s00531⁃016⁃1441⁃x Zong, K. Q., Klemd, R., Yuan, Y., et al., 2017. The Assembly of Rodinia: The Correlation of Early Neoproterozoic (Ca. 900 Ma) High⁃Grade Metamorphism and Continental Arc Formation in the Southern Beishan Orogen, Southern Central Asian Orogenic Belt (CAOB). Precambrian Research, 290: 32-48. https://doi.org/10.1016/j.precamres.2016.12.010" target="_blank"> https://doi.org/10.1016/j.precamres.2016.12.010 白瑾, 1993.华北陆台北缘前寒武纪地质及铅锌成矿作用.北京:地质出版社, 47-89. 陈井胜, 邢德和, 刘淼, 等, 2017.辽宁辽阳地区辽河群酸性火山岩锆石U⁃Pb年代学及其地质意义.岩石学报, 33(9): 2792-2810. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201709010.htm 贺高品, 叶慧文, 1998.辽东-吉南地区早元古代两种类型变质作用及其构造意义.岩石学报, 28(2): 25-35. http://www.cnki.com.cn/Article/CJFDTotal-YSXB802.002.htm 李星云, 张丽华, 1990.辽河群几种主要变质岩地球化学特征.国土资源, (3): 199-211. http://www.cnki.com.cn/Article/CJFDTotal-LOAD199003001.htm 刘福来, 刘平华, 王舫, 等, 2015.胶-辽-吉古元古代造山/活动带巨量变沉积岩系的研究进展.岩石学报, 31(10): 2816-2846. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201510002 刘平华, 蔡佳, 邹雷, 2017a.辽东半岛北部三家子石榴斜长角闪岩变质演化P⁃T⁃t轨迹及其地质意义:来自相平衡模拟与锆石U⁃Pb定年的约束.岩石学报, 33 (9): 2649-2674. http://d.wanfangdata.com.cn/Periodical/ysxb98201709001 刘平华, 刘福来, 田忠华, 等, 2017b.辽东半岛辽阳-本溪地区北辽河群巴罗型变质带变质变形历史:对胶-辽-吉带古元古代造山作用过程的启示.北京: 2017中国地球科学联合学术年会. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDW201710004008.htm 刘永达, 邴志波, 董景超, 1989.辽东半岛早元古宙枕状熔岩特征.辽宁地质, (4): 206-215. http://www.cnki.com.cn/Article/CJFDTotal-LOAD198903001.htm 刘永江, 杨振升, 李三忠, 等, 1997.古元古代拉伸构造模式──以胶北、辽东和吉南地区为例.长春地质学院学报, 27 (2): 141-146. http://www.cqvip.com/QK/91256X/199702/2532358.html 卢良兆, 徐学纯, 刘福来, 1996.中国北方早前寒武纪孔兹岩系.长春:长春出版社, 195-234. 文飞, 田忠华, 刘平华, 等, 2020.辽东半岛古元古代北辽河群浪子山组巴罗式变质带分布、变质特征及其构造意义, 地球科学, 45(9): 3403-3419. https://kns.cnki.net/kcms/detail/detail.aspx?dbcode=CJFD&dbname=CJFDAUTO&filename=DQKX202009018&v=6n79NuKJ8dLQTMJsal1Qxr5SzPvbWkemZouKu%25mmd2Fd5htHLop1jeL5xsuVnzb3VT05t 杨明春, 陈斌, 闫聪, 2015.华北克拉通胶-辽-吉带古元古代条痕状花岗岩成因及其构造意义.地球科学与环境学报, 37(5): 31-51. http://www.cnki.com.cn/Article/CJFDTotal-XAGX201505004.htm 张朋, 赵岩, 寇林林, 等, 2019.辽东半岛丹东地区中生代花岗岩锆石U⁃Pb年龄、Hf同位素特征及其地质意义.地球科学, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129 张秋生, 杨振升, 1988.辽东半岛早期地壳与矿床.北京:地质出版社. 赵岩, 寇林林, 张朋, 等, 2019.辽东半岛隆昌地区~2 113 Ma变辉长岩地球化学与Hf同位素研究:对胶辽吉造山带构造演化的制约.地球科学, 44(10): 3333-3345. doi: 10.3799/dqkx.2019.185 周世泰, 1994.鞍山-本溪地区条带状铁矿地质.北京:地质出版社. -
dqkxzx-45-9-3217-附表1.xlsx
-
点击查看大图
计量
- 文章访问数: 1798
- HTML全文浏览量: 876
- PDF下载量: 92
- 被引次数: 0
