萍乐拗陷龙潭组海相泥页岩勘探潜力
|
摘要
为评价中国东南地区上古生界富有机质泥页岩勘探前景,基于区域地质背景、露头观察和地球化学测试,通过对萍乐拗陷二叠系龙潭组岩相古地理、富有机质泥页岩的有机地球化学特征及平面分布差异的系统分析,探讨富有机质泥页岩控制因素。萍乐拗陷龙潭组时期为整体海退背景下的海陆过渡潮坪沉积环境;龙潭组富有机质泥页岩厚度在平面上表现为西厚东薄;有机碳质量分数为0.06%～12.32%,高值区位于萍乡一带,表现出西高东低的特点;有机质类型主要为Ⅲ型干酪根,总体以生气为主;R_o值为0.5%～5.45%,呈现自东向西成熟度逐渐增高的趋势。萍乐拗陷龙潭组富有机质泥页岩整体质量西高东低,沉积环境、埋藏史及热事件是形成该现象的主要控制因素。对萍乐拗陷西部地区而言,埋藏和热事件影响较大;而中东部地区则主要受埋藏作用的影响。中部丰城地区具备较好的非常规油气勘探前景。
Based on the regional geological background, outcrop observation and analysis of geochemical data, the lithofacies paleogeography, organic geochemical characteristics and distribution discrepancy of the Permian Longtan Formation organic matter-rich mud shale in Pingle Depression are studied and the controlling factors of the mud shale are discussed in order to evaluate the exploration prospects of the Upper Paleozoic organic matter-rich mud shale in southeast China. Research shows that the Longtan Formation is deposited in a sedimentary environment of sea-land transition tidal flat under an overall regressive background. In the Pingle Depression, the Longtan Formation organic matter-rich shale is thick in the west and thin in the east. The distribution range of TOC of the mud shale is 0.06%～12.32% and the highest TOC value occurs in the Pingxiang area, and generally, the TOC value in the west is higher than that in the east. Organic matter types of the mud shale are mainly gas-produced Ⅲ kerogen, with a R_o distribution range of 0.5%～5.45%, and its maturity increases from east to west and the overall quality of the Longtan Formation organic matter-rich shale in the Pingle Depression is also high in the west and low in the east. It is revealed that the sedimentary environments, burial history and thermal events are the main controlling factors for the enrichment characteristics of organic materials. Of the controlling factors, burial and thermal events play an important role in the accumulation of organic materials in the western Pingle Depression, while buried history is the main controlling factor in the central and eastern regions. It is proposed that the Fengcheng area in the central Pingle Depression has a good prospect for unconventional oil and gas exploration.
Based on the regional geological background, outcrop observation and analysis of geochemical data, the lithofacies paleogeography, organic geochemical characteristics and distribution discrepancy of the Permian Longtan Formation organic matter-rich mud shale in Pingle Depression are studied and the controlling factors of the mud shale are discussed in order to evaluate the exploration prospects of the Upper Paleozoic organic matter-rich mud shale in southeast China. Research shows that the Longtan Formation is deposited in a sedimentary environment of sea-land transition tidal flat under an overall regressive background. In the Pingle Depression, the Longtan Formation organic matter-rich shale is thick in the west and thin in the east. The distribution range of TOC of the mud shale is 0.06%～12.32% and the highest TOC value occurs in the Pingxiang area, and generally, the TOC value in the west is higher than that in the east. Organic matter types of the mud shale are mainly gas-produced Ⅲ kerogen, with a R_o distribution range of 0.5%～5.45%, and its maturity increases from east to west and the overall quality of the Longtan Formation organic matter-rich shale in the Pingle Depression is also high in the west and low in the east. It is revealed that the sedimentary environments, burial history and thermal events are the main controlling factors for the enrichment characteristics of organic materials. Of the controlling factors, burial and thermal events play an important role in the accumulation of organic materials in the western Pingle Depression, while buried history is the main controlling factor in the central and eastern regions. It is proposed that the Fengcheng area in the central Pingle Depression has a good prospect for unconventional oil and gas exploration.
引文
[1] 黄孝波,李贤庆,王帅,等.江西萍乐坳陷页岩气成藏条件分析[J].中国煤炭地质,2012,24(11):17-21.Huang X B, Li X Q, Wang S, et al. Shale gas reservoir condition analysis in Pingxiang-Leping Depression, Jiangxi[J]. Coal Geology of China, 2012, 24(11): 17-21. (in Chinese)
[2] 李瑞江,付立新,杨桦,等. 江西萍乐坳陷西部下二叠统烃源岩评价[C]//第十届全国有机地球化学学术会议论文摘要汇编,2005:63-65.Li R J, Fu L X, Yang H, et al. Jiangxi Pingle Depression evaluation of hydrocarbon source rocks of Lower Permian in the western conference[C]//The 10th National Conference on Organic Geochemistry in the Assembly, 2005: 63-65. (in Chinese)
[3] 胡秋祥,邱开国,伯慧,等.江西省二叠系龙潭组煤型气烃源岩特征[J].江西煤炭科技,2015,(1):67-68.Hu Q X, Qiu K G, Bo H, et al. Characteristics of coal-related gas source rock in the Longtan Formation of Permian in Jiangxi Province[J]. Jiangxi Coal Science and Technology, 2015, (1): 67-68. (in Chinese)
[4] 许德如,王力,王智琳,等.江西萍乐凹陷构造-沉积演化的基本特征及对找煤预测的启示[J].大地构造与成矿学,2011,35(4):513-524.Xu D R, Wang L, Wang Z L, et al. Tectonic-sedimentary characteristics of the Pingxiang-Leping Depression in Jiangxi Province and its implications on coal mineral resource prospecting[J]. Geotectonica et Metallogenia, 2011, 35(4): 513-524. (in Chinese)
[5] 俞宽坤.萍乐坳陷上二叠统乐平组泥页岩储层特征[J].中国地质,2016,43(2):520-529.Yu K K. Reservoir characteristics of Upper Permian Leping Formation shale in Pingle Depression[J]. Geology in China, 2016, 43(2): 520-529. (in Chinese)
[6] 何伟相,周矿水,喻晓平,等.江西萍乐坳陷带西段早三叠世地层划分与对比及沉积环境分析[J].中国地质,2014,41(1):148-161.He W X, Zhou K S, Yu X P, et al. Stratigraphic classification and correlation and sedimentary environment analysis of the early Triassic in western Pingxiang-Leping Depression, Jiangxi Province[J]. Geology in China, 2014, 41(1): 148-161. (in Chinese)
[7] 王力,许德如,王智琳,等.江西萍乐坳陷构造演化基本特征及控煤作用分析[J].地球科学与环境学报,2010,32(增刊):120-121.Wang L, Xu D R, Wang Z L, et al. Jiangxi Pingle basin characteristic and control coal basin tectonic evolution analysis[J]. Journal of Earth Science and Environmental, 2010, 32(S): 120-121. (in Chinese)
[8] 祖辅平.中国东南部晚古生代以来典型盆地沉积构造环境演化特征[D].南京:南京大学档案馆,2012.Zu F P. Evolution Features of Sedimentary and Structural Environment of Representative Basins Since Late Palaeozoic in Southeast China[D]. Nanjing: The Archive of Nanjing University, 2012. (in Chinese)
[9] 李会军,张立勤,梁锋,等.江西萍乐坳陷海相含油气系统特征[J].新疆石油地质,2003,24(3):210-214.Li H J, Zhang L Q, Liang F, et al. Jiangxi Pingle Depression marine petroleum system characteristics[J]. Xinjiang Petroleum Geology, 2003, 24(3): 210-214. (in Chinese)
[10] 李峰.萍乐坳陷安源组岩相古地理及成煤模式研究[D].成都:成都理工大学档案馆,2017.Li F. Study on Lithofacies Paleogeography and Coal Forming Model of Anyuan Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[11] 潘博.萍乐坳陷上二叠统乐平组富有机质页岩研究[D].成都:成都理工大学档案馆,2017.Pan B. The Study of Organic-Rich Shale of the Upper Permian Leping Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[12] 孙晶,王建强,龚建明,等.下扬子陆域海相中-古生界烃源岩有机质丰度特征及其岩相古地理[J].海洋地质前沿,2016,32(1):55-59.Sun J, Wang J Q, Gong J M, et al. Abundance of organic matter in Mesozoic-Paleozoic marine source rocks of inland area of the Lower Yangtze and its bearing on lithofacies paleogeography[J]. Marine Geology Frontiers, 2016, 32(1): 55-59. (in Chinese)
[13] 吴浩,姚素平,焦堃,等.下扬子区上二叠统龙潭组页岩气勘探前景[J].煤炭学报,2013,38(5):870-876.Wu H, Yao S P, Jiao K, et al. Shale-gas exploration prospect of Longtan Formation in the Lower Yangtze area of China[J]. Journal of China Coal Society, 2013, 38(5): 870-876. (in Chinese)
[14] 李岩,王云鹏,赵长毅,等.四川盆地上三叠统须家河组烃源岩埋藏史及热演化特征[J].地质通报,2013,32(11):1798-1805.Li Y, Wang Y P, Zhao C Y, et al. Burial history and thermal evolution characteristics of source rocks of the Upper Triassic Xujiahe Formation, Sichuan Basin[J]. Geological Bulletin of China, 2013, 32(11): 1798-1805. (in Chinese)
[15] 王中鹏,张金川,孙睿,等.西页1井龙潭组海陆过渡相页岩含气性分析[J].地学前缘,2015,22(2):243-250.Wang Z P, Zhang J C, Sun R, et al. The gas-bearing characteristic analysis of the Longtan Formation transitional shale in Well Xiye 1[J]. Earth Science Frontier, 2015, 22(2): 243-250. (in Chinese)
[16] 黄第藩,李晋超.中国陆相油气生成[M].北京:石油工业出版,1982.Huang D P, Li J C. The Chinese Continental Oil and Gas Generation[M]. Beijing: Petroleum Industry Press, 1982. (in Chinese)
[17] 许怀先.石油地质实验测试技术与应用[M].北京:石油工业出版,2001.Xu H X. Petroleum Geology Experiment Testing Technology and Application[M]. Beijing: Petroleum Industry Press, 2001. (in Chinese)
[18] 廖志伟,胡文瑄,曹剑,等.下扬子皖南大隆组黑色岩系发育特征及油气资源潜力初探[J].高校地质学报,2016,22(1):138-151.Liao Z W, Hu W X, Cao J, et al. A preliminary investigation of the development and hydrocarbon potential of the black shales in the Upper Permian Dalong Formation, southern Anhui Province in the Lower Yangtze Region, China[J]. Geological Journal of China Universities, 2016, 22(1): 138-151. (in Chinese)
[19] 柳广弟.石油地质学[M].北京:石油工作出版社,2008.Liu G D. Petroleum Geology[M]. Beijing: Petroleum Industry Press, 2008. (in Chinese)
[20] 李炳弢.萍乐坳陷中二叠统小江边组岩相古地理及烃源岩研究[D].成都:成都理工大学档案馆,2017.Li B T. Study on Lithofacies Paleogeography and Source Rock of the Middle Permian Xiaojiangbian Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[21] 徐振宇,方朝刚,滕龙,等.金衢盆地上白垩统金华组湖相页岩油气地质特征[J].中国地质调查,2017,4(6):9-14.Xu Z Y, Fang C G, Teng L, et al. Geological characteristics of lacustrine shale oil and gas of Jinhua Formation in Upper Cretaceous in Jinqu Basin[J]. Geological Survey of China, 2017, 4(6): 9-14. (in Chinese)
[22] 李洪涛,宋之光,邹艳荣,等.冀北-辽西早白垩世沉积有机质特征与古气候环境演变[J].地质学报,2008,82(1):72-76.Li H T, Song Z G, Zou Y R, et al. Characteristics of sedimentary organic matter and paleoclimate and environmental evolution during early Cretaceous time in northern part of Hebei and western of Liaoning Provinces[J]. Acta Geologica Sinica, 2008, 82(1): 72-76. (in Chinese)
[23] 杨剑,易发成,钱壮志.黔北下寒武统黑色岩系古地温及其指示意义[J].沉积与特提斯地质,2009,29(1):87-94.Yang J, Yi F C, Qian Z Z. Study of paleotemperature of the Lower Cambrian black shale series and their implications in northern Guizhou Province[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 87-94. (in Chinese)
[24] 尹志胜.江西省富有机质页岩层系构造埋藏史与页岩气富集[D].徐州:中国矿业大学档案馆,2015.Yin Z S. Tectonic and Burial History of Organic Matter Rich Shale Formations and Shale Gas Enrichment in Jiangxi Province[D]. Xüzhou: The Archive of China University of Mining and Technology, 2015. (in Chinese)
[25] 田纹全.塔里木盆地孔雀河地区埋藏史[D].长春:吉林大学档案馆,2005.Tian W Q. Burial History of Kongque River Region in Tarim Basin[D]. Changchun: The Archive of Jilin University, 2005. (in Chinese)
[26] 邓平,舒良树,杨明桂,等.赣江断裂带地质特征及其动力学演化[J].地质论评,2003,49(2):113-122.Deng P, Shu L S, Yang M G, et al. Geological features and dynamic evolution of the Ganjiang Fault in Jiangxi Province[J]. Geological Review, 2003, 49(2): 113-122. (in Chinese)
[27] 梁兴,吴根耀.赣江断裂带中生代的的演化及其地球动力学背景[J].地质科学,2006,41(1):64-80.Liang X, Wu G Y. Mesozoic evolution of the Ganjiang Fault zone and related geodynamic settings[J]. Geological Sciences, 2006, 41(1): 64-80. (in Chinese)
[28] 梁兴,巫向阳,叶舟,等.南鄱阳盆地含油气保存单元及评价[J].天然气工业,2004,24(10):10-13.Liang X, Wu X Y, Ye Z, et al. Hydrocarbon-bearing preservation united marine facies source rocks in south Poyang superposition basin and its evaluation[J]. Natural Gas Industry, 2004, 24(10): 10-13. (in Chinese)
[29] 周松源,张介辉,徐克定,等.赣江断裂带对南鄱阳坳陷成盆的控制作用[J].天然气工业,2005,25(2):24-27.Zhou S Y, Zhang J H, Xu K D, et al. Ganjiang fault zone in south Poyang Depression into the control action of basin[J]. Natural Gas Industry, 2005, 25(2): 24-27. (in Chinese)
[30] 梁兴,叶舟,吴根耀,等.鄱阳盆地构造-沉积特征及其演化史[J].地质科学,2006,41(3):404-429.Liang X, Ye Z, Wu G Y, et al. Poyang basin structure, sedimentary characteristics and its evolution[J]. Geological Sciences, 2006, 41(3): 404-429. (in Chinese)
[31] 傅昭仁,李紫金,郑大瑜.湘赣边区NNE向走滑造山带构造发展样式[J].地学前缘,1999,6(4):263-272.Fu Z R, Li Z J, Zheng D Y. The Xianggan border area NNE to develop in the strike-slip orogenic belt tectonic style[J]. Earth Science Frontiers, 1999, 6(4): 263-272. (in Chinese)
[32] 崔学军,陈祥云,楼法生,等.赣江断裂带的特征及其与郯庐断裂带的关系[J].地学前缘,2002,9(4):339-340.Cui X J, Chen X Y, Lou F S, et al. The characteristics of the Ganjiang fault zone and its relationship with the Tanlu fault zone[J]. Earth Science Frontiers, 2002, 9(4): 339-340. (in Chinese)
[33] 崔学军,夏斌,曾佐勋,等.赣江断裂与郯庐断裂接合作用及其成矿意义[J].大地构造与成矿学,2004,28(1):1-7.Cui X J, Xia B, Zeng Z X, et al. Junction between Ganjiang fault and Tanlu fault and its significance to mineralization[J]. Geotectonica et Metallogenia, 2004, 28(1): 1-7. (in Chinese)
[2] 李瑞江,付立新,杨桦,等. 江西萍乐坳陷西部下二叠统烃源岩评价[C]//第十届全国有机地球化学学术会议论文摘要汇编,2005:63-65.Li R J, Fu L X, Yang H, et al. Jiangxi Pingle Depression evaluation of hydrocarbon source rocks of Lower Permian in the western conference[C]//The 10th National Conference on Organic Geochemistry in the Assembly, 2005: 63-65. (in Chinese)
[3] 胡秋祥,邱开国,伯慧,等.江西省二叠系龙潭组煤型气烃源岩特征[J].江西煤炭科技,2015,(1):67-68.Hu Q X, Qiu K G, Bo H, et al. Characteristics of coal-related gas source rock in the Longtan Formation of Permian in Jiangxi Province[J]. Jiangxi Coal Science and Technology, 2015, (1): 67-68. (in Chinese)
[4] 许德如,王力,王智琳,等.江西萍乐凹陷构造-沉积演化的基本特征及对找煤预测的启示[J].大地构造与成矿学,2011,35(4):513-524.Xu D R, Wang L, Wang Z L, et al. Tectonic-sedimentary characteristics of the Pingxiang-Leping Depression in Jiangxi Province and its implications on coal mineral resource prospecting[J]. Geotectonica et Metallogenia, 2011, 35(4): 513-524. (in Chinese)
[5] 俞宽坤.萍乐坳陷上二叠统乐平组泥页岩储层特征[J].中国地质,2016,43(2):520-529.Yu K K. Reservoir characteristics of Upper Permian Leping Formation shale in Pingle Depression[J]. Geology in China, 2016, 43(2): 520-529. (in Chinese)
[6] 何伟相,周矿水,喻晓平,等.江西萍乐坳陷带西段早三叠世地层划分与对比及沉积环境分析[J].中国地质,2014,41(1):148-161.He W X, Zhou K S, Yu X P, et al. Stratigraphic classification and correlation and sedimentary environment analysis of the early Triassic in western Pingxiang-Leping Depression, Jiangxi Province[J]. Geology in China, 2014, 41(1): 148-161. (in Chinese)
[7] 王力,许德如,王智琳,等.江西萍乐坳陷构造演化基本特征及控煤作用分析[J].地球科学与环境学报,2010,32(增刊):120-121.Wang L, Xu D R, Wang Z L, et al. Jiangxi Pingle basin characteristic and control coal basin tectonic evolution analysis[J]. Journal of Earth Science and Environmental, 2010, 32(S): 120-121. (in Chinese)
[8] 祖辅平.中国东南部晚古生代以来典型盆地沉积构造环境演化特征[D].南京:南京大学档案馆,2012.Zu F P. Evolution Features of Sedimentary and Structural Environment of Representative Basins Since Late Palaeozoic in Southeast China[D]. Nanjing: The Archive of Nanjing University, 2012. (in Chinese)
[9] 李会军,张立勤,梁锋,等.江西萍乐坳陷海相含油气系统特征[J].新疆石油地质,2003,24(3):210-214.Li H J, Zhang L Q, Liang F, et al. Jiangxi Pingle Depression marine petroleum system characteristics[J]. Xinjiang Petroleum Geology, 2003, 24(3): 210-214. (in Chinese)
[10] 李峰.萍乐坳陷安源组岩相古地理及成煤模式研究[D].成都:成都理工大学档案馆,2017.Li F. Study on Lithofacies Paleogeography and Coal Forming Model of Anyuan Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[11] 潘博.萍乐坳陷上二叠统乐平组富有机质页岩研究[D].成都:成都理工大学档案馆,2017.Pan B. The Study of Organic-Rich Shale of the Upper Permian Leping Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[12] 孙晶,王建强,龚建明,等.下扬子陆域海相中-古生界烃源岩有机质丰度特征及其岩相古地理[J].海洋地质前沿,2016,32(1):55-59.Sun J, Wang J Q, Gong J M, et al. Abundance of organic matter in Mesozoic-Paleozoic marine source rocks of inland area of the Lower Yangtze and its bearing on lithofacies paleogeography[J]. Marine Geology Frontiers, 2016, 32(1): 55-59. (in Chinese)
[13] 吴浩,姚素平,焦堃,等.下扬子区上二叠统龙潭组页岩气勘探前景[J].煤炭学报,2013,38(5):870-876.Wu H, Yao S P, Jiao K, et al. Shale-gas exploration prospect of Longtan Formation in the Lower Yangtze area of China[J]. Journal of China Coal Society, 2013, 38(5): 870-876. (in Chinese)
[14] 李岩,王云鹏,赵长毅,等.四川盆地上三叠统须家河组烃源岩埋藏史及热演化特征[J].地质通报,2013,32(11):1798-1805.Li Y, Wang Y P, Zhao C Y, et al. Burial history and thermal evolution characteristics of source rocks of the Upper Triassic Xujiahe Formation, Sichuan Basin[J]. Geological Bulletin of China, 2013, 32(11): 1798-1805. (in Chinese)
[15] 王中鹏,张金川,孙睿,等.西页1井龙潭组海陆过渡相页岩含气性分析[J].地学前缘,2015,22(2):243-250.Wang Z P, Zhang J C, Sun R, et al. The gas-bearing characteristic analysis of the Longtan Formation transitional shale in Well Xiye 1[J]. Earth Science Frontier, 2015, 22(2): 243-250. (in Chinese)
[16] 黄第藩,李晋超.中国陆相油气生成[M].北京:石油工业出版,1982.Huang D P, Li J C. The Chinese Continental Oil and Gas Generation[M]. Beijing: Petroleum Industry Press, 1982. (in Chinese)
[17] 许怀先.石油地质实验测试技术与应用[M].北京:石油工业出版,2001.Xu H X. Petroleum Geology Experiment Testing Technology and Application[M]. Beijing: Petroleum Industry Press, 2001. (in Chinese)
[18] 廖志伟,胡文瑄,曹剑,等.下扬子皖南大隆组黑色岩系发育特征及油气资源潜力初探[J].高校地质学报,2016,22(1):138-151.Liao Z W, Hu W X, Cao J, et al. A preliminary investigation of the development and hydrocarbon potential of the black shales in the Upper Permian Dalong Formation, southern Anhui Province in the Lower Yangtze Region, China[J]. Geological Journal of China Universities, 2016, 22(1): 138-151. (in Chinese)
[19] 柳广弟.石油地质学[M].北京:石油工作出版社,2008.Liu G D. Petroleum Geology[M]. Beijing: Petroleum Industry Press, 2008. (in Chinese)
[20] 李炳弢.萍乐坳陷中二叠统小江边组岩相古地理及烃源岩研究[D].成都:成都理工大学档案馆,2017.Li B T. Study on Lithofacies Paleogeography and Source Rock of the Middle Permian Xiaojiangbian Formation in Pingle Depression[D]. Chengdu: The Archive of Chengdu University of Technology, 2017. (in Chinese)
[21] 徐振宇,方朝刚,滕龙,等.金衢盆地上白垩统金华组湖相页岩油气地质特征[J].中国地质调查,2017,4(6):9-14.Xu Z Y, Fang C G, Teng L, et al. Geological characteristics of lacustrine shale oil and gas of Jinhua Formation in Upper Cretaceous in Jinqu Basin[J]. Geological Survey of China, 2017, 4(6): 9-14. (in Chinese)
[22] 李洪涛,宋之光,邹艳荣,等.冀北-辽西早白垩世沉积有机质特征与古气候环境演变[J].地质学报,2008,82(1):72-76.Li H T, Song Z G, Zou Y R, et al. Characteristics of sedimentary organic matter and paleoclimate and environmental evolution during early Cretaceous time in northern part of Hebei and western of Liaoning Provinces[J]. Acta Geologica Sinica, 2008, 82(1): 72-76. (in Chinese)
[23] 杨剑,易发成,钱壮志.黔北下寒武统黑色岩系古地温及其指示意义[J].沉积与特提斯地质,2009,29(1):87-94.Yang J, Yi F C, Qian Z Z. Study of paleotemperature of the Lower Cambrian black shale series and their implications in northern Guizhou Province[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(1): 87-94. (in Chinese)
[24] 尹志胜.江西省富有机质页岩层系构造埋藏史与页岩气富集[D].徐州:中国矿业大学档案馆,2015.Yin Z S. Tectonic and Burial History of Organic Matter Rich Shale Formations and Shale Gas Enrichment in Jiangxi Province[D]. Xüzhou: The Archive of China University of Mining and Technology, 2015. (in Chinese)
[25] 田纹全.塔里木盆地孔雀河地区埋藏史[D].长春:吉林大学档案馆,2005.Tian W Q. Burial History of Kongque River Region in Tarim Basin[D]. Changchun: The Archive of Jilin University, 2005. (in Chinese)
[26] 邓平,舒良树,杨明桂,等.赣江断裂带地质特征及其动力学演化[J].地质论评,2003,49(2):113-122.Deng P, Shu L S, Yang M G, et al. Geological features and dynamic evolution of the Ganjiang Fault in Jiangxi Province[J]. Geological Review, 2003, 49(2): 113-122. (in Chinese)
[27] 梁兴,吴根耀.赣江断裂带中生代的的演化及其地球动力学背景[J].地质科学,2006,41(1):64-80.Liang X, Wu G Y. Mesozoic evolution of the Ganjiang Fault zone and related geodynamic settings[J]. Geological Sciences, 2006, 41(1): 64-80. (in Chinese)
[28] 梁兴,巫向阳,叶舟,等.南鄱阳盆地含油气保存单元及评价[J].天然气工业,2004,24(10):10-13.Liang X, Wu X Y, Ye Z, et al. Hydrocarbon-bearing preservation united marine facies source rocks in south Poyang superposition basin and its evaluation[J]. Natural Gas Industry, 2004, 24(10): 10-13. (in Chinese)
[29] 周松源,张介辉,徐克定,等.赣江断裂带对南鄱阳坳陷成盆的控制作用[J].天然气工业,2005,25(2):24-27.Zhou S Y, Zhang J H, Xu K D, et al. Ganjiang fault zone in south Poyang Depression into the control action of basin[J]. Natural Gas Industry, 2005, 25(2): 24-27. (in Chinese)
[30] 梁兴,叶舟,吴根耀,等.鄱阳盆地构造-沉积特征及其演化史[J].地质科学,2006,41(3):404-429.Liang X, Ye Z, Wu G Y, et al. Poyang basin structure, sedimentary characteristics and its evolution[J]. Geological Sciences, 2006, 41(3): 404-429. (in Chinese)
[31] 傅昭仁,李紫金,郑大瑜.湘赣边区NNE向走滑造山带构造发展样式[J].地学前缘,1999,6(4):263-272.Fu Z R, Li Z J, Zheng D Y. The Xianggan border area NNE to develop in the strike-slip orogenic belt tectonic style[J]. Earth Science Frontiers, 1999, 6(4): 263-272. (in Chinese)
[32] 崔学军,陈祥云,楼法生,等.赣江断裂带的特征及其与郯庐断裂带的关系[J].地学前缘,2002,9(4):339-340.Cui X J, Chen X Y, Lou F S, et al. The characteristics of the Ganjiang fault zone and its relationship with the Tanlu fault zone[J]. Earth Science Frontiers, 2002, 9(4): 339-340. (in Chinese)
[33] 崔学军,夏斌,曾佐勋,等.赣江断裂与郯庐断裂接合作用及其成矿意义[J].大地构造与成矿学,2004,28(1):1-7.Cui X J, Xia B, Zeng Z X, et al. Junction between Ganjiang fault and Tanlu fault and its significance to mineralization[J]. Geotectonica et Metallogenia, 2004, 28(1): 1-7. (in Chinese)
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |