Stratigraphic Subdivision and Correlation of the Mesozoic in the Bohai Bay Basin
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摘要: 渤海湾盆地中生界长期缺乏统一的岩石地层格架.基于测井、录井、孢粉组合及年龄数据分析，开展了地层划分和对比研究.研究表明，中生界可划分为8个岩石地层单元：（1）三叠系陆相红层，发育Aratrisporites⁃Triassisporis⁃Chordasporites组合，最大沉积年龄为（241.4±6.8）Ma至（248.2±1.9）Ma；（2）侏罗系含煤地层，发育Cyathidites⁃Osmundacidites⁃Cycadopites⁃Classopollis组合，最大沉积年龄为（173.4±1.1）Ma至（187.2±4.8）Ma；（3）侏罗系灰色砂岩层，发育Cyathidites⁃Osmundacidites⁃Deltoidospora⁃Cycadopites组合，最大沉积年龄为（155.3±1.3）Ma至（164.4±3.8）Ma；（4）侏罗系红色砂砾岩层，发育Classopollis⁃Abietineaepollenites组合；（5）下白垩统下部含基性火山岩红层，发育Cicatricosisporites⁃Lygodiumsporites⁃Classopollis组合；火山岩年龄在140~132 Ma之间；（6）下白垩统中部含中、基性火山岩灰色地层，发育Lygodiumsporites⁃Cicatricosisporites⁃Osmundacidites⁃Cycadopites组合，火山岩年龄在130~116 Ma之间；（7）下白垩统上部含中、基性火山岩地层，发育Cicatricosisporites⁃Schizaeoisporites⁃Classopollis⁃Piceites组合，火山岩年龄在119~103 Ma之间；（8）上白垩统含酸性火山岩红层，发育Schizaeoisporites⁃Ephedripites⁃Classopollis组合，火山岩年龄在76~69 Ma之间.Abstract: The Mesozoic in the Bohai Bay basin lacks unified stratigraphic framework. Based on logging data, sporopollen assemblage and age analysis of clastic and volcanic rocks, the stratigraphic subdivision and correlation of the Mesozoic were studied. The Mesozoic strata can be divided into eight stratigraphic units. The Triassic continental red strata develops the Aratrisporites⁃Triassisporis⁃Chordasporites assemblage, and the maximum depositional ages range from (241.4±6.8) Ma to (248.2±1.9) Ma. The Cyathidites⁃Osmundacidites⁃Cycadopites⁃Classopollis assemblage forms in the Jurassic coal-bearing strata, and the maximum depositional ages of the strata are from (173.4±1.1) Ma to (187.2±4.8) Ma. For the Jurassic gray sandstone strata, the maximum depositional ages range from (155.3±1.3) Ma to (164.4±3.8) Ma and the Cyathidites⁃Osmundacidites⁃Deltoidospora⁃Cycadopites assemblage are developed. The Jurassic red sandstone and gravel strata develop the Classopollis⁃Abietineaepollenites assemblage. In early stage of early Cretaceous, the red clastic strata with basic volcanic rock and the Cicatricosisporites⁃Lygodiumsporites⁃Classopollis assemblage formed. The volcanic rocks ages are from 140 to 132 Ma. For the gray clastic strata with intermediate-basic volcanic rock in the middle part of the lower Cretaceous, the Lygodiumsporites⁃Cicatricosisporites⁃Osmundacidites⁃Cycadopites assemblage and the volcanic rocks of the ages from 130 to 116 Ma are developed. The clastic strata with intermediate-basic volcanic rock in the upper part of the lower Cretaceous develop the assemblage of Cicatricosisporites⁃Schizaeoisporites⁃classopollis⁃Piceites, and the volcanic rocks ages range from 119 to 103 Ma. The Schizaeoisporites⁃Ephedripites⁃Classopollis assemblage forms in the Upper Cretaceous red clastic strata with acidic volcanic rock ranging from 76 to 69 Ma in age.
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图 1 渤海湾盆地地理及构造位置
据Qi and Yang（2010）、李三忠等（2010）、王德英等（2019）修改. 冀中坳陷：1. 北京凹陷；2. 大兴凸起；3. 大厂凹陷；4. 宝坻凸起；5. 王草庄凸起；6. 廊固凹陷；7. 武清凹陷；8. 杨村斜坡；9.徐水凹陷；10. 容城凸起；11. 牛北斜坡；12. 牛驼镇凸起；13. 霸县凹陷；14. 文安斜坡；15. 保定凹陷；16. 高阳低凸起；17. 蠡县斜坡；18. 饶阳凹陷；19. 饶阳中央隆起带；20. 深泽低凸起；21. 深县凹陷；22. 石家庄凹陷；23. 无极藁城低凸起；24. 晋县凹陷；25. 束鹿凹陷；26. 束鹿西斜坡.沧县隆起：27. 大城凸起；28. 双窑凸起；29. 白塘口凹陷；30. 小韩庄凸起；31. 兴城凸起；32. 里坦凹陷；33. 阜城凹陷；34. 献县凸起.邢蘅隆起：35. 宁晋凸起；36. 隆尧凸起；37. 新河凸起；38. 前磨头凹陷；39. 明化镇凸起；40. 武城凸起.临清坳陷：41. 内丘凹陷；42. 巨鹿凹陷；43. 广宗低凸起；44. 南宫凹陷；45. 大营镇凹陷；46. 德州凹陷；47. 冠县凹陷；48. 堂邑低凸起；49. 莘县凹陷；50. 馆陶低凸起；51. 丘县凹陷；52. 成安低凸起；53. 邯郸凹陷；54. 汤阴凹陷；55. 东濮凹陷；56. 东濮西部斜坡；57. 东濮中央隆起带.内黄隆起：58. 楚旺凸起；59. 元村集凹陷；60. 南乐凸起.黄骅坳陷：61. 宁河断阶；62. 河西凸起；63. 涧河凹陷；64. 老王庄凸起；65. 西南庄‒柏各庄凸起；66. 乐亭凹陷；67. 姜各庄凸起；68. 昌黎凹陷；69. 马头营凸起；70. 南堡凹陷；71. 北塘凹陷；72. 塘沽低凸起；73. 板桥凹陷；74. 歧口凹陷；75. 沈青庄低凸起；76. 北大港低凸起；77. 歧北凹陷；78. 南大港低凸起；79. 歧南凹陷；80. 埕北斜坡；81. 沧东凹陷；82. 孔店凸起；83. 黄骅低凸起；84. 常庄凹陷；85. 盐北凹陷；86. 盐山低凸起；87. 王官屯低凸起；88. 南皮凹陷；89. 徐黑凸起；90. 盐南凹陷；91. 东光低凸起；92. 吴桥凹陷.埕宁隆起：93. 宁津凸起；94. 无槺凸起；95. 庆云凸起；96. 埕子口凸起；97. 埕北凹陷；98. 埕北低凸起；99. 沙南凹陷；100. 沙垒田凸起.济阳坳陷：101. 惠民凹陷；102. 惠民中央隆起带；103. 曲提地垒；104. 惠民南部斜坡；105. 林攀家低凸起；106. 青城凸起；107. 滨县凸起；108. 东营凹陷；109. 东营中央隆起带；110. 青东凹陷；111. 广饶凸起；112. 潍北凸起S；113. 莱南凹陷；114. 潍北凸起N；115. 莱州湾凹陷；116. 莱北低凸起；117. 黄河口凹陷；118. 长堤—孤岛低凸起；119. 孤北低凸起；120.垦东凸起；121. 青坨子凸起；122. 陈家庄凸起；123. 沾化凹陷；124. 义和庄凸起；125. 车镇凹陷.昌维坳陷：126. 牛头镇凹陷；127. 寿光凸起；128. 侯镇凹陷；129.昌乐凹陷；130. 朱留店凸起；131. 潍坊凹陷；132. 潍县凸起；133. 潍北凹陷.渤中坳陷：134. 秦南凹陷；135. 石臼坨凸起；136. 渤中凹陷；137. 渤南低凸起；138. 渤东低凸起；139. 渤东凹陷；140. 庙西北凸起；141. 庙西南凸起；142. 庙西凹陷.辽东湾坳陷：143. 辽西凹陷；144. 辽西南凸起；145. 辽西凸起；146. 辽中凹陷；147. 辽东凸起；148. 辽东凹陷.辽河坳陷：149. 西部凸起；150. 西部凹陷；151. 中央凸起；152. 东部凹陷；153. 东部凸起；154. 大民屯凹陷
Fig. 1. Geography and structural position of the Bohai Bay basin
图 2 渤海湾盆地中生界岩性地层及其测井响应特征
a. 冀中坳陷，杨村斜坡，GE1井；b. 冀中坳陷，文安斜坡，SU49井；c. 冀中坳陷，无极藁城低凸起，JI2井；d. 临清坳陷，东濮凹陷，QG2井；e. 临清坳陷，丘县凹陷，QIU4井；f. 黄骅坳陷，东光低凸起，DG1井；g. 黄骅坳陷，埕北斜坡，ZH4井；h. 黄骅坳陷，王官屯低凸起，NV82井；i. 黄骅坳陷，北大港低凸起，GANG59井；j. 黄骅坳陷，孔店凸起，FENG22-15井；k. 济阳坳陷，埕北低凸起，ZG17井；l. 济阳坳陷，东营凹陷，WANG111井；m. 渤中坳陷，秦南凹陷，QHD30-1井；n. 辽河坳陷，西部凹陷，XG1井；o. 辽河坳陷，西部凹陷，SONG1井
Fig. 2. Characteristics of Mesozoic lithostratigraphiy and its logging response of the Bohai Bay basin
图 3 渤海湾盆地中生界孢粉聚类图
样品序号见附表2
Fig. 3. Cluster plot of Mesoic sporopollen in the Bohai Bay basin
图 4 渤海湾盆地中生界孢粉主成分分析双标图
Fig. 4. Biplot of principle component analysis of Mesozoic sporopollen in the Bohai Bay basin
图 5 渤海湾盆地侏罗系含煤地层（a）、侏罗系灰色砂岩层（b）、下白垩统中部含中、基性火山岩灰色地层（c）和下白垩统上部含中、基性火山岩地层（d）的孢粉主成分分析双标图
Fig. 5. Biplot of principle component analysis of sporopollen Jurassic coal beds (a), Jurassic grey sandstone beds (b), middle volcanic rocks of the Lower Cretaceous (c), and Upper volcanic rocks of the Lower Cretaceous (d) in the Bohai Bay basin
图 6 渤海湾盆地中生界孢粉和地层单元对应图
Fig. 6. Correspondence plot of Mesoic sporopollen and stratigraphy in the Bohai Bay basin
图 7 渤海湾盆地中生界主要孢粉含量变化
BB. 渤海湾盆地；JZ. 冀中坳陷；LQ. 临清坳陷；HH. 黄骅坳陷；JY. 济阳坳陷；BZ. 渤中坳陷；LH. 辽河坳陷
Fig. 7. The variation of Mesozoic main sporopollen content in the Bohai Bay basin
图 8 渤海湾盆地中生界砂岩及火山岩典型锆石CL图像及年龄（Ma）
Fig. 8. Cathodoluminescence images and ages (Ma) of Mesozoic sandstone and volcanic rock in the Bohai Bay basin
图 9 渤海湾盆地中生界碎屑岩锆石年龄分布、火山岩锆石协和图和加权平均年龄
Fig. 9. Age distribution of detrital zircons, concordant zircons and weighted average ages of volcanic rocks in the Bohai Bay basin
图 10 渤海湾盆地中生界碎屑岩锆石最大沉积年龄(Ma)
Bio. 孢粉地层年龄（Ma）
Fig. 10. Maximum depositional ages (Ma) of zircons from Mesozoic clastic rocks in the Bohai Bay basin
图 12 渤海湾盆地中生界综合地层格架
小岩性柱状图表示地层分布范围有限;年龄数据上标文献: 1. 蒋飞虎等(2006);2. 本次研究; 3. 朱吉昌等(2020); 4. Li et al. (2013); 5. Zhang et al. (2011); 6. Jin et al. (2020); 7. 任云飞等(2013); 8. 郭永峰(2012); 9. 李涵(2019); 10. 刘华(2014); 1. 吴庆勋等(2017); 12. Sun et al. (2017)
Fig. 12. Mesozoic integrated stratigraphic framework of the Bohai Bay basin
表 1 渤海湾盆地中生界火山岩年龄及碎屑岩最大沉积年龄统计
Table 1. Ages of Mesozoic volcanic rocks and maximum depositional age of Mesozoic clastic rocks in the Bohai Bay basin
层位 地区 井号 深度（m） 岩性 测试方法 年龄（Ma） 出处 上白垩统含酸性火山岩红层 黄骅坳陷 F22-15 2 944.36 安山岩 LA-ICP-MS 69.95±0.78 朱吉昌等，2020 黄骅坳陷 F22-15 2 950 流纹岩 SHRIMP 71.5±2.6 Zhang et al., 2011 黄骅坳陷 ZAO1532 2 778.00 安山岩 LA-ICP-MS 72.0±1.9 Jin et al., 2020 黄骅坳陷 ZAO1532 2 946.80 火山碎屑岩 LA-ICP-MS 73.30±1.60 朱吉昌等，2020 黄骅坳陷 F22-15 2 956.00 安山岩 LA-ICP-MS 74.89±0.96 朱吉昌等，2020 黄骅坳陷 ZAO55 2 994 安山岩 LA-ICP-MS 75.77±2.03 Jin et al., 2020 下白垩统上部含中、基性火山岩地层 济阳坳陷 ZHUANG14 2 665.39 玄武岩 LA-ICP-MS 102.6±1.6 李涵，2020 济阳坳陷 KD18 1 168.98 安山岩 LA-ICP-MS 104±1.0 李涵，2020 渤中坳陷 BH6 ? 中基性火山岩 LA-ICP-MS 107.9±3.0 吴庆勋等，2017 黄骅坳陷 YANG23 1 525.30 沉凝灰岩 LA-ICP-MS 111.46±0.76 朱吉昌等，2020 黄骅坳陷 KOU23 ? 安山岩 LA-ICP-MS 111.8±0.9 任云飞等，2013 黄骅坳陷 XIAN6 2 174.50 流纹质角砾凝灰岩 LA-ICP-MS 111.90±1.00 朱吉昌等，2020 黄骅坳陷 KOU23 ? 安山岩 LA-ICP-MS 114±2.8 郭永峰，2012 黄骅坳陷 QG101 3 198 玄武岩 LA-ICP-MS 114.1±1.4 Jin et al., 2020 渤中坳陷 BH11 ? 中酸性火山岩 LA-ICP-MS 114.4±2.5 吴庆勋等，2017 渤中坳陷 BH8 ? 中酸性火山岩 LA-ICP-MS 115.1±2.1 吴庆勋等，2017 黄骅坳陷 QG101 3 150 安山岩 LA-ICP-MS 115.6±4.7 Jin et al., 2020 渤中坳陷 BH2 ? 中性火山岩 LA-ICP-MS 115.7±2.1 吴庆勋等，2017 黄骅坳陷 QG8 3 373 安山岩 LA-ICP-MS 116±1.4 Jin et al., 2020 冀中坳陷 JI2 2 502.1 凝灰岩 LA-ICP-MS 117.1±2.2 本次研究 黄骅坳陷 QG1601 2 775.90 凝灰质岩屑砂岩 LA-ICP-MS 117.7±1.50 朱吉昌等，2020 渤中坳陷 BZ13 ? 酸性火山岩 LA-ICP-MS 117.8±1.2 张震等，2019 渤中坳陷 BH1 ? 中性火山岩 LA-ICP-MS 117.8±1.2 吴庆勋等，2017 渤中坳陷 BH12 ? 中性火山岩 LA-ICP-MS 118.0±2.0 吴庆勋等，2017 黄骅坳陷 ZAO26 2 502.65 含凝灰质砂质砾岩 LA-ICP-MS 118.5±1.10 朱吉昌等，2020 黄骅坳陷 KOU36 1 686 响岩 LA-ICP-MS 118.8±1.0 Zhang et al., 2011 渤中坳陷 BH4 ? 中性火山岩 LA-ICP-MS 118.8±2.1 吴庆勋等，2017 下白垩统中部含中、基性火山岩灰色地层 辽河坳陷 TUO32 ? 酸性火山岩 LA-ICP-MS 121±2 Sun et al., 2017 黄骅坳陷 TUO36 ? 安山岩 LA-ICP-MS 121.7±3.6 郭永峰，2012 辽河坳陷 TUO33 ? 酸性火山岩 LA-ICP-MS 122±1 Sun et al., 2017 渤中坳陷 BH3 ? 中性火山岩 LA-ICP-MS 122.0±2.9 吴庆勋等，2017 渤中坳陷 BH5 ? 基性火山岩 LA-ICP-MS 122.1±2.8 吴庆勋等，2017 黄骅坳陷 KOU36 ? 粗安岩 LA-ICP-MS 122.1±3.1 任云飞等，2013 黄骅坳陷 XIAN6 1 776.40 安山岩 LA-ICP-MS 122.2±1.90 朱吉昌等，2020 渤中坳陷 BH7 ? 基性火山岩 LA-ICP-MS 122.8±5.0 吴庆勋等，2017 黄骅坳陷 XIAN6 2 171.35 流纹质角砾凝灰岩 LA-ICP-MS 123.10±1.90 朱吉昌等，2020 黄骅坳陷 KOU36 1 685.69 安山岩 LA-ICP-MS 123.40±2.20 朱吉昌等，2020 济阳坳陷 ZG27 2 986 沉积岩 自生伊利石K-Ar 123.54±1.11 刘华，2014 渤中坳陷 BZ29-9-A 2 960~2 971 凝灰岩 LA-ICP-MS ~124 赵梦等，2019 渤中坳陷 BH9 ? 基性火山岩 LA-ICP-MS 125.1±2.0 吴庆勋等，2017 渤中坳陷 BH10 ? 基性火山岩 LA-ICP-MS 128.1±3.0 吴庆勋等，2017 济阳坳陷 ZHUANG105 3 495.5 沉积岩 自生伊利石K-Ar 129.01±1.06 刘华，2014 下白垩统下部含基性火山岩红层 黄骅坳陷 KOU51 3 178 火成岩混合样 LA-ICP-MS 132±2 郭永峰，2012 黄骅坳陷 QG2 ? 玄武岩 LA-ICP-MS 133±2.0 任云飞等，2013 黄骅坳陷 QG2 ? 安山玄武岩 LA-ICP-MS 133±2.0 郭永峰，2012 黄骅坳陷 QG2 2 325.00 玄武岩 LA-ICP-MS 140.1±1.4 Jin et al., 2020 辽河坳陷 QG2 ? 中性火山岩 LA-ICP-MS 162±1？ Sun et al., 2017 辽河坳陷 DG102 ? 中性火山岩 LA-ICP-MS 163±1？ Sun et al., 2017 辽河坳陷 DG102 ? 中性火山岩 LA-ICP-MS 165±2？ Sun et al., 2017 侏罗系灰色砂岩层 黄骅坳陷 NV19 3 125.50 砂岩 LA-ICP-MS 155.3±1.3 本次研究 黄骅坳陷 TC1-1 ？ 沉积岩 LA-ICP-MS 162.5±1.6 Li et al., 2013 黄骅坳陷 YE21 3 516.86 砂岩 LA-ICP-MS 163.0±4.1 朱吉昌等，2020 黄骅坳陷 WANG22-1 3 390.96 长石岩屑砂岩 LA-ICP-MS 164.0±6.0 朱吉昌等，2020 黄骅坳陷 GUAN142 2 588.50 砂岩 LA-ICP-MS 164.4±3.8 本次研究 济阳坳陷 ZG181 3 540 沉积岩 自生伊利石K-Ar 166.22±2.16 刘华，2014 侏罗系含煤地层 济阳坳陷 ZHUANG181 3 097 沉积岩 自生伊利石K-Ar 172.12±1.29 刘华，2014 黄骅坳陷 YE21 3 744.01 砂岩 LA-ICP-MS 173.4±1.1 朱吉昌等，2020 济阳坳陷 ZHUANG119 3 884 砂岩 伊利石KAr 175.07±1.12 刘华，2014 黄骅坳陷 C4-5 2 785.3 砂岩 LA-ICP-MS 187.2±4.8 本次研究 济阳坳陷 ZG17 3 672 沉积岩 自生伊利石K-Ar 188.04±1.19 刘华，2014 三叠系陆相红层 临清坳陷 GUAN1 ? 砂岩 自生伊利石K-Ar 239.9±3.0 蒋飞虎等，2006 黄骅坳陷 ZAO1532 2 969.31 砂岩 LA-ICP-MS 248.2±1.9 朱吉昌等，2020 黄骅坳陷 DG1 1 602.20 砂岩 LA-ICP-MS 241.4±6.8 朱吉昌等，2020 
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