高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征

牛杏,  杨香华,  李丹,  常吟善,  胡孝林,  许晓明

downloadPDF
文章导航 > 沉积学报  > 2014 >  32(6): 1188-1200
牛杏, 杨香华, 李丹, 常吟善, 胡孝林, 许晓明. North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征[J]. 沉积学报, 2014, 32(6): 1188-1200.
引用本文: 牛杏, 杨香华, 李丹, 常吟善, 胡孝林, 许晓明. North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征[J]. 沉积学报, 2014, 32(6): 1188-1200.
shu
NIU Xing, YANG Xiang-hua, LI Dan, CHANG Yin-shan, HU Xiao-lin, XU Xiao-ming. The Transformation of Triassic Sedimentary Framework and Corresponding Source Rock, North Carnarvon Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1188-1200.
Citation: NIU Xing, YANG Xiang-hua, LI Dan, CHANG Yin-shan, HU Xiao-lin, XU Xiao-ming. The Transformation of Triassic Sedimentary Framework and Corresponding Source Rock, North Carnarvon Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1188-1200.
shu

North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征

  • 1.

    中国地质大学构造与油气资源教育部重点实验室 武汉 430074;

  • 2.

    中国地质大学资源学院 武汉 430074;

  • 3.

    中国海洋石油研究总院 北京 100027

基金项目: 国家科技重大专项子课题“澳大利亚西北陆架油气成藏条件及勘探潜力研究”(编号:2011ZX05030-02-02)资助
详细信息
    作者简介:

    牛杏 女 1989年出生 硕士研究生 盆地沉积学、层序地层学及储层预测 E-mail:whdidazk@163.com

    通讯作者:

    杨香华 男 教授 E-mail:xhyang111@vip.sina.com

  • 中图分类号: TE121.3;TE122.1+13

The Transformation of Triassic Sedimentary Framework and Corresponding Source Rock, North Carnarvon Basin

  • 1.

    Key Laboratory of Tectonics and Petroleum Resources(China University of Geosciences), Ministry of Education, Wuhan 430074;

  • 2.

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074;

  • 3.

    CNOOC Research Institute International Department in Beijing, Beijing 100027

    摘要
  • 摘要: North Carnarvon盆地是澳大利亚最主要的产油气盆地,也是世界上主要的富气盆地之一.三叠纪North Carnarvon盆地属于克拉通边缘坳陷,地层厚度巨大且平面分布广.中三叠世晚期澳大利亚西北陆架发生强制性海退,造成North Carnarvon盆地沉积格局发生转变,沉积环境由滨浅海突变为海陆过渡环境,从而沉积了两套差异性明显的地层,即Locker shale 和Mungaroo组.本文从宏观和微观、有机与无机入手,阐述了Locker shale 和Mungaroo组的古地理背景、沉积充填演化及其相关的烃源岩与有机质显微组分发育特征.
    宏观上,Mungaroo组发育大型三角洲,中粗粒分支流水道砂岩与暗色泥岩频繁互层,其中近端三角洲平原泥岩厚度较薄,薄煤层只局部发育,陆源有机质含量较高,平均TOC含量为1.59%;远端三角洲平原泥岩厚度较大,薄煤层广泛发育,陆源有机质含量高,TOC含量最高,达4.11%;三角洲前缘泥岩厚度较大,陆源有机质含量低,TOC含量低,为1.05%.Locker Shale以滨浅海相沉积为主,局部发育小型三角洲,其中开阔浅海亚相烃源岩厚度较大,前三角洲、滨浅海、开阔浅海三个亚相TOC含量相当,平均值为1.16%.
    微观上,Mungaroo组由近端平原亚相—远端平原亚相—前缘亚相壳质组含量逐渐增多,镜质组先增加后下降,惰质组先减少后增加;远端三角洲平原镜质组含量最高.Locker shale由前三角洲相—浅海相壳质组增加,镜质组和惰质组均减少.
    研究区三叠系烃源岩及有机质显微组分的分布规律与特提斯南缘特殊的古地理、季风洪水的古气候背景密切相关,Mungaroo组的远端三角洲平原为最有利的烃源岩发育环境. North Carnarvon 盆地三叠系岩相古地理格局与沉积充填演化规律体现了温室气候效应下阵发性水流主导的沉积特色,为类似地质背景下油气资源评价提供了新的思路.
    Abstract: The North Carnarvon basin is Australia's most important oil and gas basin, also one of main gas- rich basins in the world. In Triassic, North Carnarvon basin belongs to pericratonic depression and the strata are hugely thick and widely distributed. Mandatory regression occurred in northwest shelf of Australia in Late middle Triassic, causing the transformation of Triassic sedimentary framework, North Carnarvon basin, and the depositional environment of North Carnarvon basin from offshore turn into the transition facies, thus two distinct strata-Locker shale and Mungaroo group deposited in North Carnarvon basin. In this article, paleogeographic setting of Locker shale and Mungaroo group and characteristics of associated source rock and organic maceral are elaborated under macro-micro scales, and organic-inorganic aspects.
    On a macro level, Mungaroo group is dominated by large-scale delta interbedded distributary channel sandstones and dark mudstones. The mudstone in proximal delta plain is thin, of which terrigenous organic matter content is high and TOC content can be up to 1.59%, besides, thin coal seams just developed locally. The mudstone in remote delta plain is thick, of which terrigenous organic matter content is high and TOC content is highest and can be up to 4.11%, besides, thin coal seams developed widely. The mudstone in delta front is thick, of which terrigenous organic matter content is low and TOC content can be up to 1.05%. Locker Shale is composed of major shallow sea depositional association and small-scale delta. The source rock in open shallow sea subfacies is the thick, what's more, prodelta, offshore and open shallow sea subfacies TOC content is much lower, and three sub-phases average TOC is 1.16%.
    On a micro level, sedimentary facies of Mungaroo group from the proximal plain facies-distal plain facies-front subfacies liptinite content gradually increased, with that vitrinite first increased and then decreased, but inertinite first decreased and then increased. As Locker Shale, by the prodelta to neritic facies liptinite increased, with that both vitrinite and inertinite reduced.
    The distribution of source rocks and organic maceral is closely related to special paleogeographic and monsoon flood paleoclimate setting of the southern margin of Thethys. The distal delta plain of Mungaroo group is the most favorable environment for the development of source rock. Lithofacies palaeogeographic framework and Sedimentary evolution regularity in Trassic of North Carnarvon Basin reflect the sedimentary characteristics which is dominated by paroxysmal water under the effect of greenhouse climate, providing a new train of thought for oil and gas resource evaluation in a similar geological setting.
    • HTML全文
    • 参考文献(29)
  • [1] 白国平,殷进垠. 澳大利亚北卡那封盆地油气地质特征及勘探潜力分析[J]. 石油实验地质,2007,29(3):253-258[Bai Guoping, Yin Jinyin. Petroleum geological features and exploration potential analyses of North Carnavon Basin, Australia[J]. Petroleum Geology & Experaiment, 2007, 29(3): 253-258]
    [2] 张建球,钱桂华,郭念发,等. 澳大利亚大型沉积盆地与油气成藏[M]. 北京:石油工业出版社,2008:88-103[Zhang Jinqiu, Qian Guihua, Guo Nianfa, et al. Large Sedimentary Basins and Hydrocarbon Accumulation of Australia[M]. Beijing: Petroleum Industry Press, 2008: 88-103]
    [3] Nereo Preto, Evelyn Kustatscher, Paul B. Wignall. Triassic climates — State of the art and perspectives[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 290(1/2/3/4): 1-10
    [4] Hallam A. A review of Mesozoic climate[J]. Journal of the Geological Society of London, 1985, 142(3): 433-445
    [5] Pindell J. Mesozoic-cenozoic paleogeographic evolution of northern south-America [J]. AAPG Bulletin, 1993, 77(2): 340
    [6] Russell F. Dubiel, Judith Totman Parrish, J. Michael Parrish, et al. The Pangaean megamonsoon — Evidence from the Upper Triassic Chinle Formation, Colorado Plateau [J]. Palaios, 1991, 6(4): 347-370
    [7] Wang P X. Global monsoon in a geological perspective[J]. Chinese Science Bulletin, 2009, 54(7): 1113-1136
    [8] Kidder D L, Worsley T R. Causes and consequences of extreme Permo-Triassic warming to globally equable climate and relation to the Permo-Triassic extinction and recovery[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 203(3/4): 207-237
    [9] Frakes L A, Francis J E. A guide to Phanerozoic polar climates from high-latitude ice-rafting in the Cretaceous [J]. Nature, 1988, 333(6173): 547-549
    [10] N. Rubeen Cunneo, Edith L, Taylor T N, et al. In situ fossil forest from the upper Fremouw Formation (Triassic) of Antarctica: paleoenvironmental setting and paleoclimate analysis [J]. Paleogeography, Paleoclimatology, Paleoecology, 2003, 197(3): 239-261
    [11] Nicoletta Buratti, Simonetta Cirilli. Microfloristic provincialism in the Upper Triassic Circum-Mediterranean area and palaeogeographic implication [J]. Geobios, 2007, 40(2): 133-142
    [12] Tao Chongzhi, Bai Guoping, Liu Junlan,et al. Mesozoic lithofacies palaeogeography and petroleum prospectivity in North Carnarvon Basin, Australia[J]. Journal of Palaeogeography, 2013, 2(1): 81-92
    [13] 刘本培,冯庆来,Chonglakmani,等. 滇西古特提斯多岛洋的结构及其南北延伸[J]. 地学前缘,2002,9(3):161-170[Liu Benpei, Feng Qinglai, Chonglakmani, et al. The structure and north-south extension of the poly-island Paleotethys Ocean in Western Yunnan[J]. Earth Science Frontiers, 2002, 9(3): 161-170]
    [14] 殷鸿福,吴顺宝,杜远生,等. 华南是特提斯多岛洋体系的一部分[J]. 地球科学,1999,24(1):1-12[Yin Hongfu, Wu Shunbao, Du Yuansheng, et al. South China defined as part of Tethyan archipelagic ocean system[J]. Earth Science, 1999, 24(1): 1-12]
    [15] 颜佳新. 东特提斯地区二叠—三叠纪古气候特征及其古地理意义[J]. 地球科学,1999,24(1):13-20[Yan Jiaxin. Permian-Triassic ancient climate characteristics and the palaeogeographic significance of East Tethys region[J]. Earth Science, 1999, 24(1): 13-20]
    [16] 王飞宇,傅家谟,刘德汉,等. 煤和陆源有机质生油岩有机岩石学特点及评价[J]. 新疆石油地质,1994,15(1):22-29[Wang Feiyu, Fu Jiamo, Liu Dehan, et al. Organic petrology characteristics and evaluation of coal and terrestrial organic matter oil source rocks[J]. Xinjiang Petroleum Geology, 1994, 15 (1): 22-29]
    [17] 朱伟林,李建平,周心怀,等. 渤海新近系浅水三角洲沉积体系与大型油气田勘探[J]. 沉积学报,2008,26(2):575-582[Zhu Weilin, Li Jianping, Zhou Xinhuai, et al. Neogene shallow water delta sedimentary system and large hydrocarbon exploration of Bohai[J]. Acta Sedimentologica Sinica, 2008, 26(2): 575-582]
    [18] 邓运华. 论河流与油气的共生关系[J]. 石油学报,2010,31(1):12-17[Deng Yunhua. Analysis on correlation of river and petroleum[J]. Acta Petrolei Sinica, 2010, 31(1): 12-17]
    [19] 李增学,魏久传,余继峰,等. 煤地质学[M]. 北京:地质出版社,2009 [Li Zengxue, Wei Jiuchuan, Yu Jifeng, et al. Coal Geology[M]. Beijing: Geological Publishing House, 2009]
    [20] 冯杨伟,屈红军,张功成. 澳大利亚西北陆架深水盆地油气地质特征[J]. 海洋地质与第四纪地质,2011,31(4):131-140[Feng Yangwei, Qu Hongjun, Zhang Gongcheng, et al. Hydrocarbon geological characteristics of Australia's northwest continental shelf deep-water basin[J]. Marine Geology & Quateranry Geology, 2011, 31(4): 131-140]
    [21] Cook A C, Michelle Smyth, Vos R G. Source potential of upper Triassic Fluvio-Deltaic systems of the Exmouth Plateau[J]. The APEA Journal, 1985
    [22] 刘聪. 澳大利亚北卡那封盆地层序地层特征及对海平面变化的响应[D]. 北京:中国地质大学(北京),2011:12-85[Liu Cong. Stratigraphy characteristics and response of sea level change of Australia's North Carnarvon Basin sequence[D]. Beijing: China University of Geosciences(Beijing), 2011: 12-85]
    [23] Lister T R, Orbell G. Triassic-Jurassic source rock studies in the North Carnarvon Basin[J]. 1974
    [24] 张家青. 澳大利亚西北大陆架油气地质特征及勘探潜力——以北卡那封盆地为例[J]. 内蒙古石油化工,2011(9):186-189[Zhang Jiaqing. Hydrocarbon geological characteristics and exploration potential of Australia's north west continental shelf - North Carnarvon Basin as an example[J]. Inner Mongolia Petrochemical Industry, 2011(9): 186-189]
    [25] 冯杨伟,屈红军,张功成,等. 澳大利亚西北陆架中生界生储盖组合特征[J]. 海洋地质动态,2010,26(6):16-23[Feng Yangwei, Qu Hongjun, Zhang Gongcheng, et al. Mesozoic source-reservoir-seal assemblage characteristics in the northwest shelf of Australia [J]. Marine Geology Letters, 2010, 26(6): 16-23]
    [26] 王全伟,阚泽忠,刘啸虎,等. 四川中生代陆相盆地孢粉组合所反映的古植被与古气候特征[J]. 四川地质学报,2008,28(2):89-95[Wang Quanwei, Kan Zezhong, Liu Xiaohu, et al. The Mesozoic sporopollen assemblage in the Sichuan Basin and its significance to paleovegetation and paleoclimate[J]. Sichuan Geology, 2008, 28(2): 89-95]
    [27] 徐兆辉,胡素云,汪泽成,等. 古气候恢复及其对沉积的控制作用——以四川盆地上三叠统须家河组为例[J]. 沉积学报,2011,29(2):235-244[Xu Zhaohui, Hu Suyun, Wang Zecheng, et al. Restoration of paleoclimate and its geological significance: As an example from upper Triassic Xujiahe Formation in Sichuan Basin[J]. Acta Sedimentologica Sinica, 2011, 29(2): 235-244]
    [28] 鲁胜梅,黄其胜. 川东地区晚三叠世须家河植物群及其沉积环境[J]. 地球科学,1992,17(3):329-335[Lu Shengmei,Huang Qisheng. Late Triassic epoch Xujiahe flora and its sedimentary environment in the east region of Sichuan [J]. Earth Science, 1992, 17(3):329-335]
    [29] Jan Golonka. Late Triassic and Early Jurassic palaeogeography of the world [J]. Palaogeography, Palaeoclimatology, Palaeoecology, 2007, 244(1/2/3/4): 297-307
    • 相关文章
  • [1] 张莹, 陈少平, 刘志峰, 杨东升, 耿名扬, 吴斌.  沉积环境对渤海金西A洼烃源岩的控制作用 . 沉积学报, 2023, 41(3): 890-900. doi: 10.14027/j.issn.1000-0550.2022.047
    [2] 孔令武, 赵红岩, 梁建设, 程涛, 王嘉, 赵佳奇, 喻英梅.  转换大陆边缘盆地深水浊积砂岩油气成藏差异性研究 . 沉积学报, 2022, 40(1): 244-254. doi: 10.14027/j.issn.1000-0550.2020.084
    [3] 赵鹏, 彭光荣, 吴静, 许新明, 熊万林, 石创, 蔡国富, 张月霞.  珠一坳陷小型洼陷文昌组烃源岩发育模式与主控因素 . 沉积学报, 2022, 40(4): 1109-1121. doi: 10.14027/j.issn.1000-0550.2021.081
    [4] 袁灵聪, 朱晓军, 蔡进功, 钟锴.  东海盆地长江坳陷美人峰组烃源岩沉积环境与生烃潜力评价 . 沉积学报, 2021, 39(2): 506-514. doi: 10.14027/j.issn.1000-0550.2020.016
    [5] 陈治军, 王志伟, 张少清, 高怡文, 韩长春, 李科社.  二连盆地宝勒根陶海凹陷烃源岩生物标志化合物特征与油源对比 . 沉积学报, 2020, 38(2): 451-462. doi: 10.14027/j.issn.1000-0550.2019.034
    [6] 占王忠, 谭富文.  羌塘盆地晚三叠世岩相古地理特征与烃源岩 . 沉积学报, 2020, 38(4): 876-885. doi: 10.14027/j.issn.1000-0550.2019.093
    [7] 刘得光, 周路, 李世宏, 马万云, 郭文建.  玛湖凹陷风城组烃源岩特征与生烃模式 . 沉积学报, 2020, 38(5): 946-955. doi: 10.14027/j.issn.1000-0550.2020.005
    [8] 朱扬明, 李颖, 郝芳, 邹华耀, 郭旭升.  四川盆地海、陆相烃源岩有机质稳定碳同位素组成变化及其地球化学意义 . 沉积学报, 2017, 35(6): 1254-1264. doi: 10.14027/j.cnki.cjxb.2017.06.016
    [9] 王成, 王万春, 王建丰, 樊海龙.  鄂尔多斯盆地奥陶系烃源岩支链烷烃特征及其地质意义 . 沉积学报, 2017, 35(4): 853-862. doi: 10.14027/j.cnki.cjxb.2017.04.019
    [10] 储呈林, 陈强路, 张博, 史政, 姜海健, 杨鑫.  热液活动对东二沟剖面玉尔吐斯组烃源岩形成的影响 . 沉积学报, 2016, 34(4): 803-810. doi: 10.14027/j.cnki.cjxb.2016.04.020
    [11] 赵青芳, 李双林, 温珍河, 龚建明, 肖国林, 吴亮亮.  北黄海盆地LV井侏罗系烃源岩特征及油源对比 . 沉积学报, 2016, 34(4): 794-802. doi: 10.14027/j.cnki.cjxb.2016.04.019
    [12] 陈方文, 卢双舫, 丁雪.  松辽盆地齐家—古龙凹陷中浅层烃源岩生烃量评价 . 沉积学报, 2014, 32(6): 1181-1187.
    [13] .  湘鄂西寒武系烃源岩地球化学特征与沉积环境分析 . 沉积学报, 2013, 31(6): 1122-1132.
    [14] 樊 馥.  孙吴—嘉荫盆地太平林场组烃源岩海侵特征研究 . 沉积学报, 2009, 27(4): 650-656.
    [15] 郭建军.  塔里木盆地寒武系烃源岩的研究新进展 . 沉积学报, 2008, 26(3): 518-524.
    [16] 陈文彬.  北羌塘盆地布曲组烃源岩生物标志物特征及意义 . 沉积学报, 2007, 25(5): 808-814.
    [17] 孟仟祥, 房嬛, 徐永昌, 沈平.  柴达木盆地石炭系烃源岩和煤岩生物标志物特征及其地球化学意义 . 沉积学报, 2004, 22(4): 729-736.
    [18] 郭泽清, 钟建华, 刘卫红, 杨树锋, 陈汉林.  应用EASY% R_o法模拟柴达木盆地西部烃源岩成熟史 . 沉积学报, 2004, 22(1): 154-160.
    [19] 刘洛夫, 康永尚, 齐雪峰, 唐勇, 熊正祥.  准噶尔盆地侏罗系层序地层格架中的烃源岩评价 . 沉积学报, 2002, 20(4): 687-694.
    [20] 李金有, 朴明植, 肖乾华.  几种煤、油共生盆地的烃源岩演化模式 . 沉积学报, 1997, 15(2): 109-113.
    • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  821
  • HTML全文浏览量:  0
  • PDF下载量:  1065
  • 被引次数: 0
出版历程
  • 收稿日期:  2013-11-20
  • 修回日期:  2014-02-24
  • 刊出日期:  2014-12-10

目录

    North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征

    • 1. 中国地质大学构造与油气资源教育部重点实验室 武汉 430074;
    • 2. 中国地质大学资源学院 武汉 430074;
    • 3. 中国海洋石油研究总院 北京 100027
      • 基金项目:  国家科技重大专项子课题“澳大利亚西北陆架油气成藏条件及勘探潜力研究”(编号:2011ZX05030-02-02)资助
      作者简介:

      牛杏 女 1989年出生 硕士研究生 盆地沉积学、层序地层学及储层预测 E-mail:whdidazk@163.com

      通讯作者: 杨香华 男 教授 E-mail:xhyang111@vip.sina.com
    • 收稿日期: 2013-11-20
    • 修回日期: 2014-02-24
    • 刊出日期: 2014-12-10

    • 中图分类号: TE121.3;TE122.1+13

    摘要: North Carnarvon盆地是澳大利亚最主要的产油气盆地,也是世界上主要的富气盆地之一.三叠纪North Carnarvon盆地属于克拉通边缘坳陷,地层厚度巨大且平面分布广.中三叠世晚期澳大利亚西北陆架发生强制性海退,造成North Carnarvon盆地沉积格局发生转变,沉积环境由滨浅海突变为海陆过渡环境,从而沉积了两套差异性明显的地层,即Locker shale 和Mungaroo组.本文从宏观和微观、有机与无机入手,阐述了Locker shale 和Mungaroo组的古地理背景、沉积充填演化及其相关的烃源岩与有机质显微组分发育特征.
    宏观上,Mungaroo组发育大型三角洲,中粗粒分支流水道砂岩与暗色泥岩频繁互层,其中近端三角洲平原泥岩厚度较薄,薄煤层只局部发育,陆源有机质含量较高,平均TOC含量为1.59%;远端三角洲平原泥岩厚度较大,薄煤层广泛发育,陆源有机质含量高,TOC含量最高,达4.11%;三角洲前缘泥岩厚度较大,陆源有机质含量低,TOC含量低,为1.05%.Locker Shale以滨浅海相沉积为主,局部发育小型三角洲,其中开阔浅海亚相烃源岩厚度较大,前三角洲、滨浅海、开阔浅海三个亚相TOC含量相当,平均值为1.16%.
    微观上,Mungaroo组由近端平原亚相—远端平原亚相—前缘亚相壳质组含量逐渐增多,镜质组先增加后下降,惰质组先减少后增加;远端三角洲平原镜质组含量最高.Locker shale由前三角洲相—浅海相壳质组增加,镜质组和惰质组均减少.
    研究区三叠系烃源岩及有机质显微组分的分布规律与特提斯南缘特殊的古地理、季风洪水的古气候背景密切相关,Mungaroo组的远端三角洲平原为最有利的烃源岩发育环境. North Carnarvon 盆地三叠系岩相古地理格局与沉积充填演化规律体现了温室气候效应下阵发性水流主导的沉积特色,为类似地质背景下油气资源评价提供了新的思路.

    English Abstract

    牛杏, 杨香华, 李丹, 常吟善, 胡孝林, 许晓明. North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征[J]. 沉积学报, 2014, 32(6): 1188-1200.
    引用本文: 牛杏, 杨香华, 李丹, 常吟善, 胡孝林, 许晓明. North Carnarvon盆地三叠系沉积格局转换与烃源岩发育特征[J]. 沉积学报, 2014, 32(6): 1188-1200.
    shu
    NIU Xing, YANG Xiang-hua, LI Dan, CHANG Yin-shan, HU Xiao-lin, XU Xiao-ming. The Transformation of Triassic Sedimentary Framework and Corresponding Source Rock, North Carnarvon Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1188-1200.
    Citation: NIU Xing, YANG Xiang-hua, LI Dan, CHANG Yin-shan, HU Xiao-lin, XU Xiao-ming. The Transformation of Triassic Sedimentary Framework and Corresponding Source Rock, North Carnarvon Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1188-1200.
    shu

      全文HTML

    参考文献 (29)

    目录

      /

      返回文章
      返回

      友情链接

      期刊在线

      联系我们

      • 网站版权 © 2011《沉积学报》编辑部
      • 地址: 兰州市天水中路8号
      • 邮编: 730000   Tel:（0931）8264231
      • 陇ICP备2021001824号-28
      • 甘公网安备 62010202000673号
      关注微信公众号

      Email alert

      RSS

      系统由 北京仁和汇智信息技术有限公司 设计集成    百度统计

      x 关闭 永久关闭

      2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）