ANALYSIS ON THE URANIUM METALLOGENIC CONDITIONS OF SIFANGTAI FORMATION IN TAIKANG AREA, SONGLIAO BASIN
-
摘要:
通过对泰康地区的铀源条件、构造条件、含矿建造地质特征以及氧化-还原条件等方面进行研究，综合分析了泰康地区四方台组砂岩型铀矿的成矿条件，认为盆地西部和北部的富铀岩体为其提供丰富的铀源，四方台组具有成矿所必需的泥-砂-泥结构，良好的补-径-排水文体系以及良好的氧化-还原条件.四方台组底部砂体中获得铀工业孔和铀矿化孔，显示出泰康地区四方台组在砂岩型铀成矿勘探方面具有较好的前景，找矿类型为层间氧化带型.
Abstract:Through the study of uranium source condition, tectonic setting, geological characteristics of ore-bearing formation and oxidation-reduction condition in Taikang area, the paper analyzes the metallogenic conditions of sandstone uranium deposit in Sifangtai Formation. It is considered that the uranium-rich rocks in the west and north of Songliao Basin provide abundant uranium source. The Sifangtai Formation necessarily has a mud-sand-mud structure, a good recharge-runoff-discharge system and oxidation-reduction condition for mineralization. The uranium industrial holes and mineralized holes are obtained in the sand body at the bottom of Sifangtai Formation, indicating a good prospect in mineralization and exploration of sandstone uranium with the prospecting type of interlayer oxidation zone.
-
Key words:
- Sifangtai Formation /
- metallogenic condition /
- sandstone uranium deposit /
- Taikang area /
- Songliao Basin
-
-
[1] 宋鹰. 松辽盆地裂后期构造反转及其动力学背景分析[D]. 武汉: 中国地质大学, 2010: 1-137.
Song Y. The post-rift tectonic inversion of Songliao Basin, NE China and its dynamic background[D]. Wuhan: China University of Geosciences, 2010: 1-137.
[2] 焦养泉, 吴立群, 彭云彪, 等. 中国北方古亚洲构造域中沉积型铀矿形成发育的沉积-构造背景综合分析[J]. 地学前缘, 2015, 22(1): 189-205. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501018.htm
Jiao Y Q, Wu L Q, Peng Y B, et al. Sedimentary-tectonic setting of the deposition-type uranium deposits forming in the Paleo-Asian tectonic domain, North China[J]. Earth Science Frontiers, 2015, 22(1): 189-205. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501018.htm
[3] 王丹丹, 赵松, 张文浩, 等. 松辽盆地外围通化地区高精度重磁电特征及其构造格架[J]. 中国地质, 2020, 47(4): 1056-1068. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202004012.htm
Wang D D, Zhao S, Zhang W H, et al. Lithofacies identification and deep structure of Tonghua area in the periphery of Songliao Basin based on high-precision gravity-magnetic electrical survey[J]. Geology in China, 2020, 47(4): 1056-1068. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202004012.htm
[4] 朱筱敏, 康安, 王贵文. 陆相坳陷型和断陷型湖盆层序地层样式探讨[J]. 沉积学报, 2003, 21(2): 283-287. doi: 10.3969/j.issn.1000-0550.2003.02.015
Zhu X M, Kang A, Wang G W. Sequence stratigraphic models of depression and faulted-down lake basins[J]. Acta Sedimentologica Sinica, 2003, 21(2): 283-287. doi: 10.3969/j.issn.1000-0550.2003.02.015
[5] 叶德燎. 松辽盆地东南隆起区下白垩统层序地层格架及油气成藏规律[J]. 地质科学, 2005, 40(2): 227-236. doi: 10.3321/j.issn:0563-5020.2005.02.007
Ye D L. Lower cretaceous sequence stratigraphic framework and hydrocarbon accumulation in the Southeast Rise, Songliao Basin, China[J]. Chinese Journal of Geology, 2005, 40(2): 227-236. doi: 10.3321/j.issn:0563-5020.2005.02.007
[6] 张振强, 桑吉盛, 金成洙. 松辽盆地东南隆起区反转构造对砂岩型铀矿成矿的作用[J]. 铀矿地质, 2006, 22(3): 151-156, 181. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200603003.htm
Zhang Z Q, Sang J S, Jin C Z. Inversion structure and its contribution to sandstone uranium metallogenesis in southeast uplifted domain of Songliao basin[J]. Uranium Geology, 2006, 22(3): 151-156, 181. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200603003.htm
[7] 张雷, 王英民, 李树青, 等. 松辽盆地北部四方台组-明水组高精度层序地层特征与有利区带预测[J]. 中南大学学报(自然科学版), 2009, 40(6): 1679-1688. https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD200906038.htm
Zhang L, Wang Y M, Li S Q, et al. High-resolution sequence stratigraphic characteristic and favorable hydrocarbon accumulation prediction of Sifangtai to Mingshui formation in the north of Songliao Basin[J]. Journal of Central South University (Science and Technology), 2009, 40(6): 1679-1688. https://www.cnki.com.cn/Article/CJFDTOTAL-ZNGD200906038.htm
[8] 程日辉, 王国栋, 王璞珺, 等. 松科1井北孔四方台组-明水组沉积微相及其沉积环境演化[J]. 地学前缘, 2009, 16(6): 85-95. doi: 10.3321/j.issn:1005-2321.2009.06.009
Cheng R H, Wang G D, Wang P J, et al. Sedimentary microfacies and sedimentary environment evolution of Sifangtai Formation and Mingshui Formation in SK-Ⅰ(n)[J]. Earth Science Frontiers, 2009, 16(6): 85-95. doi: 10.3321/j.issn:1005-2321.2009.06.009
[9] 万涛, 刘招君, 胡菲, 等. 松辽盆地北部上白垩统四方台组河流相层序沉积特征[J]. 大庆石油地质与开发, 2018, 37(5): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201805001.htm
Wan T, Liu Z J, Hu F, et al. Sedimentary characteristics of the fluvial sequence of upper Cretaceous Sifangtai Formation in North Songliao Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2018, 37(5): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-DQSK201805001.htm
[10] 陈路路, 聂逢君, 严兆彬. 松辽盆地西部斜坡带四方台组铀成矿条件分析[J]. 世界核地质科学, 2013, 30(2): 70-78. doi: 10.3969/j.issn.1672-0636.2013.02.002
Chen L L, Nie F J, Yan Z B. Analysis on uranium metallogenic conditions of Sifangtai Formation in western slope of Songliao Basin[J]. World Nuclear Geoscience, 2013, 30(2): 70-78. doi: 10.3969/j.issn.1672-0636.2013.02.002
[11] 封志兵, 聂逢君, 严兆彬, 等. 松辽盆地西部斜坡铀成矿条件及聚铀模式[J]. 大庆石油地质与开发, 2013, 32(4): 36-41. doi: 10.3969/J.ISSN.1000-3754.2013.04.008
Feng Z B, Nie F J, Yan Z B, et al. Mineralizing conditions and metallogenic model of uranium in west slope of Songliao Basin[J]. Petroleum Geology & Oilfield Development in Daqing, 2013, 32(4): 36-41. doi: 10.3969/J.ISSN.1000-3754.2013.04.008
[12] 李娟, 舒良树. 松辽盆地中、新生代构造特征及其演化[J]. 南京大学学报(自然科学), 2002, 38(4): 525-531. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ200204009.htm
Li J, Shu L S. Mesozoic-Cenozoic tectonic features and evolution of the Song-Liao Basin, NE China[J]. Journal of Nanjing University (Natural Science), 2002, 38(4): 525-531. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ200204009.htm
[13] 孙永河, 白鹿, 付晓飞. 松辽盆地北部T2反射层断裂密集带成因机制[J]. 地球科学——中国地质大学学报, 2013, 38(4): 797-806. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201304014.htm
Sun Y H, Bai L, Fu X F. Genetic mechanism of T2 reflector fault dense zones in Northern Songliao Basin[J]. Earth Science-Journal of China University of Geosciences, 2013, 38(4): 797-806. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201304014.htm
[14] 孙永河, 陈艺博, 孙继刚, 等. 松辽盆地北部断裂演化序列与反转构造带形成机制[J]. 石油勘探与开发, 2013, 40(3): 275-283. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201303005.htm
Sun Y H, Chen Y B, Sun J G, et al. Evolutionary sequence of faults and the formation of inversion structural belts in the northern Songliao Basin[J]. Petroleum Exploration and Development, 2013, 40(3): 275-283. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201303005.htm
[15] 何中波, 秦明宽, 宋继叶, 等. 准噶尔盆地东北部侏罗系砂岩型铀矿成矿环境与找矿方向探讨[J]. 矿床地质, 2018, 37(1): 175-190. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201801013.htm
He Z B, Qin M K, Song J Y, et al. A study of metallogenic environments and prospecting direction of Jurassic sandstone-type uranium deposit in northeastern Junggar Basin[J]. Mineral Deposits, 2018, 37(1): 175-190. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201801013.htm
[16] 李亮, 王永康, 张建晔. 在油气藏周围寻找砂岩型铀矿[J]. 西安石油学院学报(自然科学版), 2001, 16(5): 7-10. https://www.cnki.com.cn/Article/CJFDTOTAL-XASY200105002.htm
Li L, Wang Y K, Zhang J Y. Exploiting the sandstone uranite mineral deposits around oil and gas reservoirs[J]. Journal of Xi'an Petroleum Institute (Natural Science Edition), 2001, 16(5): 7-10. https://www.cnki.com.cn/Article/CJFDTOTAL-XASY200105002.htm
[17] 高瑞祺, 蔡希源. 松辽盆地油气田形成条件与分布规律[M]. 北京: 石油工业出版社, 1997: 1-9, 529-530.
Gao R Q, Cai X Y. Oil and gas fields distribution rules in Songliao Basin[M]. Beijing: Petroleum Industry Press, 1997: 1-9, 529-530. (in Chinese)
[18] 赵忠华. 中国北东部中新生代盆地地浸砂岩型铀矿成矿条件及找矿方向[J]. 地质与资源, 2003, 12(1): 36-41, 60. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract9680.shtml
Zhao Z H. Metallogenic conditions and prospecting direction for in-situ leachable sandstone-type uranium deposits in the Meso-Cenozoic basins of northeast China[J]. Geology and Resources, 2003, 12(1): 36-41, 60. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract9680.shtml
[19] 赵杰, 罗梅, 刘峰, 等. 松辽盆地北部可地浸砂岩型铀矿形成条件与分布特征[J]. 成都理工学院学报, 2002, 29(2): 137-143. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200202002.htm
Zhao J, Luo M, Liu F, et al. Formation conditions and distribution features of situ leachable sandstone-type uranium mineralization in the North of Songliao Basin[J]. Journal of Chengdu University of Technology, 2002, 29(2): 137-143. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200202002.htm
[20] 康德江, 庞雄奇, 吕延防, 等. 松辽盆地西斜坡水动力场与油气的聚集成藏[J]. 地球学报, 2008, 29(2): 205-212. doi: 10.3321/j.issn:1006-3021.2008.02.011
Kang D J, Pang X Q, Lü Y F, et al. Hydrodynamic field and hydrocarbon accumulation on the west slope of the Songliao Basin[J]. Acta Geoscientica Sinica, 2008, 29(2): 205-212. doi: 10.3321/j.issn:1006-3021.2008.02.011
[21] 焦养泉, 吴立群, 荣辉, 等. 砂岩型铀矿的双重还原介质模型及其联合控矿机理: 兼论大营和钱家店铀矿床[J]. 地球科学, 2018, 43(2): 459-474. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201802009.htm
Jiao Y Q, Wu L Q, Rong H, et al. Model of inner and outer reductive media within uranium reservoir sandstone of sandstone-type uranium deposits and its ore-controlling mechanism: Case studies in Daying and Qianjiadian uranium deposits[J]. Earth Science, 2018, 43(2): 459-474. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201802009.htm
-
下载:
图(6)
计量
- 文章访问数: 1093
- PDF下载数: 34
- 施引文献: 0