Sedimentary and Characteristics of the Denying Formation and Its Exploration Prospect in Sichuan Basin
-
摘要: 前人对四川盆地震旦系灯影组沉积格局及储层发育类型的认识存在较大分歧. 为给全盆灯影组油气勘探提供支持，利用野外剖面、钻井及地震资料，开展了灯影组沉积格局及多类型储层发育特征研究，明确了优质储层发育控制因素，指明了勘探突破有利区. 研究结果表明：（1）受绵阳-长宁裂陷槽、汉南古陆及开江-宣汉古隆起控制，灯影组发育灯二-灯四期台缘丘滩及台内丘滩4个有利相带；（2）灯四段有利丘滩相带发育受隆凹格局控制，裂陷槽控制台缘丘滩相带展布，东侧台缘相区沿南江西-元坝-阆中-高磨-栗子一带呈近南北向展布，西侧台缘相区沿威远-成都-都江堰一带呈向东凸出的弧状分布，开江-宣汉水下古隆起周缘及局部微地貌高地有利于台内丘滩大面积分布；（3）灯影组储层主要发育台缘丘滩储层及台内丘滩改造型储层，优质储层发育受高能相带、准同生期及桐湾期岩溶改造联合控制. 四川盆地灯四段发育元坝-阆中灯影组台缘、川西-栗子灯影组台缘、通南巴-普光-綦江灯影组台内3个有利勘探区，是近期灯四段深层-超深层勘探领域油气突破的重要战略新区带.Abstract: There are many divergences on the sedimentary pattern and reservoir development types of of the Sinian Dengying Formation in Sichuan Basin. In order to provide support for oil and gas exploration of Dengying Formation in the basin, the sedimentary pattern and multi type reservoir development characteristics of Dengying Formation are studied by using the field profile, drilling and seismic data. The controlling factors of high⁃quality reservoir development are defined, and the favorable areas for exploration breakthrough are pointed out. This study indicated that (1) Controlled by Mianyang⁃Changning rift trough, Hannan ancient land and Kaijiang⁃Xuanhan ancient uplift, Dengying Formation developed four favorable facies which are mound beach on the platform edge and mound beach in the platform. (2) The development of favorable dune and shoal facies belt in the fourth member of Dengying Formation is controlled by uplift depression pattern. Distribution of dune shoal facies belt on the console margin of rift trough. The platform margin facies area in the east is distributed in the Nanjiang⁃Yuanba⁃Gaomo⁃Lizi area. The platform margin facies area in the west is distributed in the Weiyuan⁃Chengdu⁃Dujiangyan area. The surrounding area of underwater paleo uplift and local micro geomorphic highland are favorable for the large⁃scale distribution of hills and beaches in the platform. (3) The reservoir of the fourth member of Dengying Formation is mainly developed in the platform margin mound bank reservoir and the shaol reformed reservoir. The development of high⁃quality reservoirs is jointly controlled by high⁃energy facies belt, quasi syngenetic period and Tongwan period karst transformation. There are three favorable exploration areas in the fourth member of Dengying Formation in Sichuan Basin: Yuanba⁃Langzhong Dengying Formation platform margin, Western Sichuan⁃Lizi Dengying Formation platform margin and Tongnanba⁃Puguang⁃Qijiang Dengying Formation platform. The three exploration areas are the important strategic new zones of oil and gas breakthrough in the deep ultra deep exploration field of the fourth member of Dengying Formation
-
图 1 川北地区构造位置及灯影组地层综合柱状图
Fig. 1. Structural location and comprehensive histogram of the fourth member of Dengying Formation in northern Sichuan
图 2 四川盆地灯二段沉积格局及沉积相平面图
Fig. 2. Sedimentary pattern and sedimentary facies plan of the secend member of Dengying Formation in Sichuan Basin
图 3 四川盆地灯四段沉积格局及沉积相平面图
Fig. 3. Sedimentary pattern and sedimentary facies plan of the fourth member of Dengying Formation in Sichuan Basin
图 4 四川盆地灯影组沉积演化模式图
格局线方向见图 3
Fig. 4. Sedimentary evolution model of Dengying Formation in Sichuan Basin
图 5 陕西宁强胡家坝剖面灯四段台缘丘滩亚相沉积特征图(据段金宝等，2019修改)
Fig. 5. Sedimentary characteristics of platform margin mound and shoal subfacies in the fourth member of Dengying Formation in Hujiaba section(modified from Duan et al., 2019)
图 6 RT1井灯四段台内丘滩亚相沉积特征图
Fig. 6. Sedimentary characteristics of inner platform shoal subfacies in the fourth member of Dengying Formation in RT1 well
图 7 四川盆地灯四段沉积及储层特征特征图
a. 陕西宁强胡家坝，裂陷槽边缘丘滩相，微生物岩发育，丘型建造，块状堆积，孔洞发育；b. 陕西宁强胡家坝，裂陷槽边缘丘滩相，藻凝块云岩，镜下见典型凝块结构，指示水体能量较强；c. 陕西宁强胡家坝，裂陷槽边缘丘滩相，藻叠层云岩，镜下见波状叠层结构，指示水体能量较强；d. YS1井，8 610 m，台缘丘滩，藻凝块云岩，藻格架孔发育，被沥青、白云石半-全充填；e. YS1井，8 644 m，台缘丘滩，藻叠层云岩，藻格架孔发育，被沥青、石英、白云石全充填；f. RT1井，8 130 m，台内丘滩，细-粉晶云岩，晶间溶孔发育；g. RT1井，台内丘滩相，藻砂屑云岩，具藻黏连结构，见溶蚀孔洞；h. RT1井，台内丘滩相，藻砂屑云岩，见溶蚀孔洞；i. RT1井，8 129.62 m，台内丘滩相，藻砂屑云岩，见溶蚀孔洞；j. 广元陈家乡，斜坡相，含云泥岩，微生物岩不发育；k. 林庵寺，斜坡相，深灰色-灰黑色块状硅质岩；l. 平武金凤，陆棚相，灯影组顶部未见岩溶改造，岩性为硅质岩夹白云岩；m. 广元东溪河，斜坡-陆棚相，灯影组上部发育硅质角砾岩滑塌沉积
Fig. 7. Sedimentary characteristics of the fourth member of Dengying Formation in Sichuan Basin
图 8 四川盆地灯四段典型沉积相地震剖面
Fig. 8. Seismic Profile of Typical Sedimentary Facies in the fourth member of Dengying Formation in Sichuan Basin
图 9 四川盆地灯四段沉积体系格架图
Fig. 9. Sedimentary facies correlation of the fourth member of Dengying Formation in Sichuan Basin
图 10 四川盆地灯影组多类型储层物性特征图
Fig. 10. Physical property characteristics of multi type reservoirs in Dengying Formation in Sichuan Basin
图 11 四川盆地灯影组岩性及沉积亚相与物性关系图
Fig. 11. Relationship between lithology, sedimentary subfacies and physical properties of Dengying Formation in Sichuan Basin
图 12 四川盆地灯四段岩溶特征图
a. CS1井，8 159.26~8 159.87 m，藻凝块、藻砂屑云岩夹泥粉晶云岩，溶蚀具有层控性及组构选择性，孔洞主要发育在微生物岩段，泥粉晶云岩段溶蚀不发育；b. 广元胡家坝，藻叠层云岩，顺藻类溶蚀；c. 广元胡家坝，藻凝块、藻砂屑云岩，花斑状溶蚀系统，孔洞发育；d. CS1井，8 159.51 m，碳酸盐岩砂和塑性角砾充填溶洞；e. 广元胡家坝，镜下溶蚀具有明显分带性，呈基岩带-半离解带-溶蚀孔洞带过渡特征，具“易碎晕”结构，单偏光；f. 旺苍鼓城，灯影组顶部见3~4 m铁质风化壳，风化壳底部溶蚀孔洞发育；g. 旺苍鼓城，风化壳2之下20 m处，溶蚀缝洞系统发育；h. JS1井，3 755 m，藻云岩、细-粉晶云岩，不规则溶洞发育
Fig. 12. Dissolution characteristics of the fourth member of Dengying Formation in Sichuan Basin
图 13 四川盆地灯影组储层岩溶作用碳氧同为素、锶同位素比值与锶含量特征图
Fig. 13. Characteristics of carbon oxygen isotope ratio, strontium isotope ratio and strontium content of reservoir karstification in Dengying Formation in Sichuan Basin
图 14 四川盆地灯四段有利勘探区评价图
Fig. 14. Evaluation map of favorable exploration area in the fourth member of Dengying Formation in Sichuan Basin
表 1 四川盆地灯四段有利勘探区评价表
Table 1. Evaluation of favorable exploration areas in the fourth member of Dengying Formation in Sichuan Basin
有利勘探区 元坝-阆中 川西-栗子 通南巴-普光-綦江 沉积环境 陡坡台缘带 缓坡台缘带 局限台地 储层类型 台缘储层 台缘储层 台内丘滩溶蚀改造储层 岩性特征 藻凝块、藻叠层、藻砂屑云岩 藻凝块、藻砂屑、细粉晶云岩 藻凝块、藻纹层、砂屑、泥粉晶云岩 储集空间 藻格架孔、粒内溶孔、粒间溶孔、晶间溶孔、
顺藻类孔洞藻格架孔、粒内溶孔、粒间溶孔、不规则溶洞 物性特征 4.58%/0.017 5 mD 4.31%/0.011 3 mD 4.07/0.000 379 mD 成岩改造 强早成岩期组构选择性溶蚀、强云化、弱海底胶结 强早成岩期组构选择性溶蚀、强云化、弱海底胶结 中强早成岩期组构选择性溶蚀、强不整合溶蚀、强云化改造、中强海底胶结 储层厚度 50~180 m 30~100 m 20~50 m 烃源岩 好/侧向供烃 较好/侧向供烃 中等/倒灌供烃 成藏模式 棚生缘储 汇聚调整 综合评价 一类有利勘探区 二类有利勘探区 
下载: 导出CSV
-
Chen, Y. N., Shen, A. J., Pan, L. Y., et al., 2017. Features, Origin and Distribution of Microbial Dolomite Reservoirs: A Case Study of 4th Member of Sinian Dengying Formation in Sichuan Basin, SW China. Petroleum Exploration and Development, 44(5): 745-757(in Chinese with English abstract). doi: 10.1016/S1876-3804(17)30085-X Davies, G. R., Smith, L. B. Jr., 2006. Structurally Controlled Hydrothermal Dolomite Reservoir Facies: An Overview. AAPG Bulletin, 90(11): 1641-1690. https://doi.org/10.1306/05220605164 Duan, J. B., Dai, L. C., Li, B. S., et al., 2019a. Reservior Characteristics and Their Controlling Factors of the Fourth Member of Upper Sinian Dengying Fm in the Northern Sichuan Basin. Natural Gas Industry, 39(7): 9-20(in Chinese with English abstract). Duan, J. B., Mei, Q. H., Li, B. S., et al., 2019b. Sinian-Early Cambrian Tectonic-Sedimentary Evolution in Sichuan Basin. Earth Science, 44(3): 738-755(in Chinese with English abstract). Fu, H. J., Yan, D. T., Yao, C. P., et al., 2022. Pore Structure and Multi-Scale Fractal Characteristics of Adsorbed Pores in Marine Shale: A Case Study of the Lower Silurian Longmaxi Shale in the Sichuan Basin, China. Journal of Earth Science, 33(5): 1278-1290. https://doi.org/10.1007/s12583-021-1602-0 Guo, H. W., Fu, M. Y., Song, R. C., et al., 2022. Algal Type and Sedimentary Model of the 4th Member, Dengying Formation in the Gaoshiti Area of Chuanzhong. Acta Sedimentologica Sinica, 40(1): 217-228(in Chinese with English abstract). He, D. F., Li, D. S., Zhang, G. W., et al., 2011. Formation and Evolution of Multicycle Superimposed Basins in Sichuan. Earth Science, 46(3): 589-606(in Chinese with English abstract). He, W. H., Tang, T. T., Le, M., L., et al., 2014. Sedimentary and Tectonics Evolution of Nanhua-Permian in South China. Earth science, 39(8): 930-953(in Chinese with English abstract). Hu, R., Li, S., Q., Wang, W., et al, 2016. Source Characteristics of Tillite the Nantuo Formation in Three Gorges, Northern Yangtze Block: Evidence from Zircon Age and Geochemical Composition. Earth Science, 41(10): 1630-1654(in Chinese with English abstract) Jin, M. D., Li, B. S., Zhu, X., et al., 2020. Characteristics and Main Controlling Factors of Reservoirs in the Fourth Member of Sinian Dengying Formation in Yuanba and its Peripheral Area, Northeastern Sichuan Basin, SW China. Petroleum Exploration and Development, 47(6): 1172-1182(in Chinese with English abstract). doi: 10.1016/S1876-3804(20)60127-1 Li, L., Tan, X. C., Zeng, W., et al., 2013. Development and Reservoir Significance of Mud Mounds in Sinian Dengying Formation, Sichuan Basin. Petroleum Exploration and Development, 40(6): 714-721(in Chinese with English abstract). doi: 10.1016/S1876-3804(13)60096-8 Li, S. J., Gao, P., Huang, B. Y., et al., 2018. Sedimentary Constraints on the Tectonic Evolution of Mianyang–Changning trough in the Sichuan Basin. Oil & Gas Geology, 39(5): 889-898(in Chinese with English abstract). Li, W., Liu, J. J., Deng, S. W., et al., 2015. The Nature and Role of Late Sinian-Early Cambrian Tectonic Movement in Sichuan Basin and Its Adjacent Areas. Acta Petrolei Sinica, 36(5): 546-556, 563(in Chinese with English abstract). Li, Z. Q., Liu, J., Li, Y., et al., 2015. Formation and Evolution of Weiyuan–Anyue Tensional Corrosion Trough in Sinian System, Sichuan Basin. Petroleum Exploration and Development, 42(1): 29-36(in Chinese with English abstract). doi: 10.1016/S1876-3804(15)60003-9 Li, Z. W., Ran, B., Xiao, B., et al., 2019. Sinian to Early Cambrian Uplift-Depression Framework along the Northern Margin of the Sichuan Basin, Central China and Its Implications for Hydrocarbon Exploration. Earth Science Frontiers, 26(1): 59-85(in Chinese with English abstract). Li, Z. X., Li, X. H., Kinny, P. D., et al., 2003. Geochronology of Neoproterozoic Syn-Rift Magmatism in the Yangtze Craton, South China and Correlations with other Continents: Evidence for a Mantle Superplume that Broke up Rodinia. Precambrian Research, 122(1/2/3/4): 85-109. https://doi.org/10.1016/s0301-9268(2)00208-5 Liu, S. G., Song, J. M., Luo, P., et al., 2016. Characteristics of Microbial Carbonate Reservoir and Its Hydrocaibon Exploring Outlook in the Sichuan Basin, China. Journal of Chengdu University of Technology (Science & Techology Editon), 42(2): 129-152(in Chinese with English abstract). doi: 10.3969/j.issn.1671-9727.2016.02.01 Liu, S. G., Sun, W., Luo, Z. L., et al., 2013. Xinkai Taphrogenesis and Petroleum Exploration from Upper Sinian to Cambrian Strata in Sichuan Basin, Chian. Journal of Chengdu University of Technology (Science & Techology Editon), 40(5): 511-520(in Chinese with English abstract). doi: 10.3969/j.issn.1671-9727.2013.05.03 Luo, B., Yang, Y. M., Luo, W. J., et al., 2015. Controlling Factors and Distribution of Reservoirs Development in Dengying Formation of Paleo-Uplift in Central Sichuan Basin. Acta Petrolei Sinica, 36(4): 416-426(in Chinese with English abstract). Mei, M. X., Zhou, P., Zhang, H., et al., 2006. Sequence Stratigraphic Framework and Its Palaeogeographical Background for the Sinian of Upper Yangtze Region. Jouranal of Palaeogeoraphy, 8(5): 219-231(in Chinese with English abstract). Merdith, A. S., Collins, A. S., Williams, S. E., et al., 2017. A Full-Plate Global Reconstruction of the Neoproterozoic. Gondwana Research, 50(4): 84-134. https://doi.org/10.1016/j.gr.2017.04.001 Wang, W. Z., Yang, Y. M., Wen, L., et al., 2016. A Study of sedimentary Characteristics of Microbial Carbonate: A Case Study of the Sinian Dengying Formation in Gaomo Area, Sichuan Basin. Geology in Chian, 43(1): 306-318(in Chinese with English abstract). Wei, G. Q., Yang, W., Xie, W. R., et al., 2022. Formation Mechanisms, Potentials and Exploration Practices of Large Lithologic Gas Reservoirs in and around an Intracratonic Rift: Taking the Sinian-Cambrian of Sichuan Basin as an Example. Petroleum Exploration and Development, 49(3): 530-545(in Chinese with English abstract). doi: 10.1016/S1876-3804(22)60044-2 Xiang, F., Chen, H. D., Zhang, J. Q., et al., 1998. Characteristics of Paleokarst Reservoir and Forecast in Sinian Dengying Formation in Ziyang Area. Natural Gas Exploration and Development, 21(4): 23-28(in Chinese with English abstract). Xiao, D., Tan, X. C., Xi, A. H., et al., 2015. Palaeokarst Characteristics of Carbonate Rocks of the Middle Permian Maokou Formation in Southern Sichuan Basin: Example of Strata-Bound Eogenetic Karst in Palaeo-Continental settings. Jouranal of Palaeogeoraphy, 17(4): 457-476(in Chinese with English abstract). Xu, Z., H., Lan, C., J., Ma, X., L., et al., 2020. Sedimentary Models and Physical Properties of Mound-Shoal Complex Reservoirs in Sinian Dengying Formation, Sichuan Basin. Earth Science, 45(4): 1281-1294(in Chinese with English abstract). Yang, W., Wei, G. Q., Zhao, R. R., et al., 2014. Characteristics and Distribution of Karst Reservoirs in the Sinian Dengying Fm, Sichuan Basin. Natural Gas Industry, 34(3): 55-60(in Chinese with English abstract). doi: 10.3787/j.issn.1000-0976.2014.03.009 Zhou, J. G., Zhang, J. Y., Deng, H. Y., et al., 2017. Lithofacies Paleogeography and Sedimentary Model of Dengying Formation of Sinian System in Sichuan Basin. Natural Gas Industry, 37(1): 24-31(in Chinese with English abstract). Zhu, D. Y., Jin, Z. J., Sun, D. S., et al., 2014. Hydrothermally Dolomitized Reservoir Bed in Sinian Dengying Formation, Northern China: an Example from Central Guizhou Uplift. Chinese Joural of Geology, 49(1): 161-175(in Chinese with English abstract). 陈娅娜, 沈安江, 潘立银, 等, 2017. 微生物白云岩储集层特征、成因和分布——以四川盆地震旦系灯影组四段为例. 石油勘探与开发, 44(5): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201705006.htm 段金宝, 代林呈, 李毕松, 等, 2019a. 四川盆地北部上震旦统灯影组四段储层特征及其控制因素. 天然气工业, 39(7): 9-20. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201907003.htm 段金宝, 梅庆华, 李毕松, 等, 2019b. 四川盆地震旦纪-早寒武世构造-沉积演化过程. 地球科学, 44(3): 738-755. doi: 10.3799/dqkx.2018.335 郭恒玮, 伏美燕, 宋荣彩, 等, 2022. 川中高石梯地区灯四段藻丘类型与沉积模式. 沉积学报, 40(1): 217-228. doi: 10.14027/j.issn.1000-0550.2020.065 何登发, 李德生, 张国伟, 等, 2011. 四川多旋回叠合盆地的形成与演化. 地质科学, 46(3): 589-606. doi: 10.3969/j.issn.0563-5020.2011.03.001 何卫红, 唐婷婷, 乐明亮, 等, 2014. 华南南华纪-二叠纪沉积大地构造演化. 地球科学, 46(3): 589-606. doi: 10.3799/dqkx.2014.087 胡蓉, 李双庆, 王伟, 等, 2016. 杨子北部三峡地区南沱组冰碛岩的物源特征: 锆石年龄和地球化学依据. 地球科学, 41(10): 1630-1654. doi: 10.3799/dqkx.2016.121 金民东, 李毕松, 朱祥, 等, 2020. 四川盆地东北部元坝及周缘地区震旦系灯影组四段储集层特征及主控因素. 石油勘探与开发, 46(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202006004.htm 李凌, 谭秀成, 曾伟, 等, 2013. 四川盆地震旦系灯影组灰泥丘发育特征及储集意义. 石油勘探与开发, 40(6): 666-672. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201306005.htm 李双建, 高平, 黄博宇, 等, 2018. 四川盆地绵阳-长宁凹槽构造演化的束缚. 石油与天然气地质, 39(5): 889-898. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201805005.htm 李伟, 刘静江, 邓胜徽, 等, 2015. 四川盆地及邻区震旦纪末-寒武纪早期构造运动性质与作用. 石油学报, 36(5): 546-556, 563. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201505003.htm 李智武, 冉波, 肖斌, 等, 2019. 四川盆地北缘震旦纪-早寒武世隆-坳格局及其油气地质意义. 地学前缘, 26(1): 59-85. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201901008.htm 李忠权, 刘记, 李应, 等, 2015. 四川盆地震旦系威远-安岳拉张侵蚀槽特征及形成演化. 石油勘探与开发, 26(1): 26-33. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201501004.htm 刘树根, 宋金民, 罗平, 等, 2016. 四川盆地深层微生物碳酸盐岩储层特征及油气勘探前景. 成都理工大学学报(自然科学版), 42(2): 129-152. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201602001.htm 刘树根, 孙玮, 罗志立, 等, 2013. 兴凯地裂运动与四川盆地下组合油气勘探. 成都理工大学学报(自然科学版), 40(5): 511-520. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201305003.htm 罗冰, 杨跃明, 罗文军, 等, 2015. 川中古隆起灯影组储层发育控制因素及展布. 石油学报, 36(4): 416-426. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201504003.htm 梅冥相, 周鹏, 张海, 等, 2006. 上杨子地区震旦系层序地层格架及其形成的古地理背景. 古地理学报, 8(5): 219-231. 王文之, 杨跃明, 文龙, 等, 2016. 微生物碳酸盐岩沉积特征研究——以四川盆地高磨地区灯影组为例. 中国地质, 43(1): 306-318. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201601023.htm 魏国齐, 杨威, 谢武仁, 等, 2022. 克拉通内裂陷及周缘大型岩性气藏形成机制、潜力及勘探实践——以四川盆地震旦-寒武系为例. 石油勘探与开发, 49(3): 465-477. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202203004.htm 向芳, 陈洪德, 张锦泉, 等, 1998. 资阳地区震旦系古岩溶储层特征及预测. 天然气勘探与开发, 21(4): 23-28. https://www.cnki.com.cn/Article/CJFDTOTAL-TRKT199804002.htm 肖笛, 谭秀成, 郗爱华, 等, 2015. 四川盆地南部中二叠统茅口组碳酸盐岩岩溶特征: 古大陆环境下层控型早成岩期岩溶实例. 古地理学报, 17(4): 457-476. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201504003.htm 徐哲航, 兰才俊, 马肖琳, 等, 2020. 四川盆地震旦系灯影组丘滩体储层沉积模式与物性特征. 地球科学, 45(4): 1281-1294. doi: 10.3799/dqkx.2019.138 杨威, 魏国齐, 赵蓉蓉, 等, 2014. 四川盆地震旦系灯影组岩溶储层特征及展布. 天然气工业, 34(3): 55-60. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201403012.htm 周进高, 张建勇, 邓红樱, 等, 2017. 四川盆地震旦系灯影组岩相古地理与沉积模式. 天然气工业, 37(1): 24-31. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG201701005.htm 朱东亚, 金之钧, 孙东胜, 等, 2014. 南方震旦系灯影组热液白云岩化及其对储层形成的影响研究. 地质科学, 49(1): 161-175. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX201401012.htm -
点击查看大图
计量
- 文章访问数: 810
- HTML全文浏览量: 916
- PDF下载量: 124
- 被引次数: 0
