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YANG Fei, LIU Yabo. 2022: Study on the influence of salt structural system on the distribution characteristics of potassium-rich brine reservoirs in Jiangling depression. Geological Bulletin of China, 41(10): 1847-1854. DOI: 10.12097/j.issn.1671-2552.2022.10.012
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A large number of salt-bearing rock systems were deposited in the Paleocene Shashi and Xinguzui group of the Jiangling depression, and various types of salt-ridge formations were formed under the influence of the Xishan movement.To clarify the distribution characteristics of potassium-rich brine in the Jiangling depression, we focus on the stratigraphic, fracture, and tectonic distribution characteristics of the Jiangling depression, and investigate the influence of the salt-ridge tectonic system on the distribution characteristics of potassium-rich brine.By analyzing the formation and evolution of the salt structure in the Jiangling Depression, it is concluded that the secondary depressions controlled by the Salt Rise Tectonics were formed at different stages of salt deposition, and brine from different stages was collected, which became the key place for salt accumulation.The potassium ions of the brine in the Jiangling depression mainly originate from the igneous rocks associated with the fractures.Potassium-rich brines are mainly distributed in the lower part of the Xinguzui group and the strata of the Shashi group, whose brine reservoirs include: sandstone reservoirs (Lijiatai area), volcanic reservoirs (Shashi and Fanjiatai area), and fracture zone reservoirs (Nangang area).The highly mineralized potassium-rich brines are widely distributed in the Jiangling depression and have a large exploration potential.
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魏琳. 江陵凹陷油气成藏条件及区带评价研究[D]. 长江大学硕士学位论文, 2020.
|
|
薛建玲, 庞振山, 程志中, 等. 深部找矿基本问题及方法[J]. 地质通报, 2020, 39(8): 1125-1136. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20200801&flag=1
|
|
尤英, 夏平, 余丽玲. 江陵凹陷沙市组蒸发岩沉积特征研究[J]. 长江大学学报(自科版), 2013, 10(2): 41-44. doi: 10.16772/j.cnki.1673-1409.2013.02.014
|
|
易积正. 江陵凹陷梅槐桥地区第三系新沟咀组下段沉积相及砂体分布研究[J]. 矿物岩石, 2010, 30(3): 77-82. doi: 10.3969/j.issn.1001-6872.2010.03.010
|
|
滕晓华, 王春连, 沈立建, 等. 江汉盆地SKD1深钻记录的古新世—始新世极热事件时期的古气候[J]. 地球学报, 2022, 43(1): 65-72. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB202201005.htm
|
|
方维萱. 论沉积盆地内成岩相系划分及类型[J]. 地质通报, 2020, 39(11): 1692-1136. doi: 10.12097/j.issn.1671-2552.2020.11.003
|
|
王春连, 刘成林, 刘宝坤, 等. 江陵凹陷古新统光卤石的发现及其钾盐找矿意义[J]. 地质学报, 2015, 89(1): 129-136. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201501010.htm
|
|
张世保. 江陵凹陷盐丘构造特征及其对油气的控制作用[J]. 江汉石油科技, 1992, (3): 1-3
|
|
高楠安. 江汉盆地江陵凹陷盐构造类型及成因机制探讨[J]. 石油地质与工程, 2013, 27(2): 9-11. doi: 10.3969/j.issn.1673-8217.2013.02.003
|
|
余小灿, 王春连, 黄华, 等. 湖北潜江凹陷古近系深层富钾卤水成因及演化[J]. 地球科学, 2022, 47(1): 122-135. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202201012.htm
|
|
周舟, 刘金帅, 周倩, 等. 江陵凹陷荆州背斜带典型构造解析[J]. 能源与环保, 2017, 39(6): 117-122. https://www.cnki.com.cn/Article/CJFDTOTAL-ZZMT201706023.htm
|
|
张黎. 江陵凹陷资福寺洼陷构造特征研究[D]. 长江大学硕士学位论文. 2012.
|
|
胡杨. 滨里海盆地东部盐构造及其对油气成藏的控制作用[J]. 内蒙古石油化工, 2014, 40(12): 1-3 https://www.cnki.com.cn/Article/CJFDTOTAL-NMSH201412001.htm
|
|
王春连, 黄华, 王九一, 等. 江陵凹陷富钾锂卤水矿田地质特征及成藏模式研究[J]. 地质学报, 2018, 92(8): 1630-1646. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201808007.htm
|
|
周惠, 田玉昆, 李娟, 等. 基于地震叠后反演与属性分析的页岩气有利储层预测[J]. 地质通报, 2021, 40(4): 557-564. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=20210412&flag=1
|
|
Wang C L, Liu C L, Wang J Y, et al. Palynology and stratigraphy of the thick evaporate-bearing Shashi Formation in Jiangling Depression, Jianghan Basin of South China, and its paleoclimate change[J]. China Geology, 2020, 2: 283-291.
|
|
Teng X H, Wang C L, Liu C L, et al. Paleocene-Eocene Thermal Maximum lacustrine sediments in deep drill core SKD1 in the Jianghan Basin: A record of enhanced precipitation in central China[J]. Global and Planetary Change, 2021, 205: 103620.
|
|
佘晓宇, 龚晓星, 吕鹏, 等. 江陵凹陷八岭山-花园多层系盐和盐泥构造及其形成机制[J]. 现代地质, 2013, 27(4): 765-773. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201304004.htm
|
|
刘卫彬, 张世奇, 李世臻, 等. 东濮凹陷沙三段储层微裂缝发育特征及意义[J]. 地质通报, 2018, 37(2/3): 496-502. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2018020327&flag=1
|
|
潘源敦, 刘成林, 徐海明. 湖北江陵凹陷深层高温富钾卤水特征及其成因探讨[J]. 化工矿产地质, 2011, 33(2): 65-72. https://www.cnki.com.cn/Article/CJFDTOTAL-HGKC201102002.htm
|
|
马黎春, 黄华, 张连元, 等. 湖北潜江凹陷古近系深层富钾卤水矿床特征及成因[J]. 地质学报, 2015, 89(11): 2114-2121. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201511023.htm
|
|
刘亚伟, 张士万, 刘涛, 等. 深层天然卤水特征及成因探讨——以江陵凹陷深层天然卤水研究为例[J]. 矿床地质, 2013, 32(6): 1291-1299. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201306016.htm
|
|
沈均均, 陈波, 王春连, 等. 江陵凹陷古近系沙市组含膏盐岩系沉积特征研究[J]. 地球学报, 2014, 35(4): 425-433. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201404005.htm
|
|
徐伟, 王宇, 李航空. 盐构造成因演化机制及其对研究钾盐矿床成因的意义[J]. 中国矿山工程, 2015, 44(2): 48-51, 70. https://www.cnki.com.cn/Article/CJFDTOTAL-YSKS201502015.htm
|
|
黄华, 袁娟梅, 彭伟, 等. 江汉盆地古近系潜江组盐湖沉积特征与成藏模式[J]. 岩性油气藏, 2021, 33(2): 9-16. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX202102002.htm
|
|
王春连, 刘成林, 胡海兵, 等. 江汉盆地江陵凹陷南缘古新统沙市组四段含盐岩系沉积特征及其沉积环境意义[J]. 古地理学报, 2012, 14(2): 165-175. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201202004.htm
|
|
刘俊, 卢明国, 童小兰, 等. 江陵凹陷构造演化与含油气系统关系研究[J]. 地球学报, 2008, (1): 89-94. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200801013.htm
|
|
余小灿, 刘成林, 王春连, 等. 江汉盆地大型富锂卤水矿床成因与资源勘查进展: 综述[J]. 地学前缘, 2022, 29(1): 107-123. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202201010.htm
|
|
王必金, 曾芳, 刘启凤, 等. 江汉盆地古潜山勘探前景展望[J]. 江汉石油学院学报, 2002, (4): 13-15. https://www.cnki.com.cn/Article/CJFDTOTAL-JHSX200204004.htm
|
|
高楠安, 陈金荣. 江陵凹陷油气成藏主控因素及勘探方向[J]. 江汉石油职工大学学报, 2012, 25(2): 4-7. https://www.cnki.com.cn/Article/CJFDTOTAL-JSZD201202004.htm
|
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