Constraints of the sequence stratigraphic structure of uranium-bearing series on mineralization in Qianjiadian uranium deposit, Songliao Basin
-
摘要: 弄清楚砂岩型铀矿含铀岩系地层结构及其对铀成矿的制约作用，是准确认识铀成矿规律和成矿作用的基础。综合地震、测井、岩心及分析测试资料，对松辽盆地西南部钱家店铀矿床含铀岩系——姚家组层序地层结构进行了研究，在此基础上，探讨了地层结构与铀成矿的关系。研究发现，钱家店地区姚家组为一个完整的三级层序，姚家组底界面为区域不整合界面，底部主要发育泥砾岩、含泥砾砂岩等，姚家组顶界为平行不整合，顶部发育一套紫红色夹灰色泥岩，在姚家组内部识别出了初始湖泛面和最大湖泛面，将其划分为低位体系域、湖泊扩展体系域和高位体系域。低位体系域分布范围较小，厚度平均约40 m，呈北东狭长型分布；湖泊扩展体系域和高位体系域地层连续超覆，分布范围向西南扩展至八仙筒-开鲁一带，总体仍为北东走向，地层平均厚度在研究区分别约为85 m和75 m。层序地层结构对研究区姚家组铀成矿具有约束作用，垂向上，由下至上不同小层序组铀矿化逐渐减弱；平面上，不同体系域铀矿化分布特征不同，低位体系域铀矿化主要发育在钱Ⅳ块-钱Ⅴ一带，呈北东走向条带状分布，矿体呈似板状、透镜状；湖泊扩展体系域铀矿化在钱Ⅱ-钱Ⅳ-钱Ⅴ一带呈不规则弧形分布，矿体呈"似卷状"，为典型的层间氧化带型铀矿化；高位体系域铀矿化主要发育在钱Ⅲ块以及南部零星分布，推测向南具有进一步找矿空间。研究结果可为研究区找矿提供依据，并为铀成矿模式及成矿过程研究提供基础。Abstract: Understanding the stratigraphic structure of uranium-bearing rock series in sandstone-type uranium deposits and its constraints on uranium mineralization is the basis of understanding the uranium metallogenic regularity and mineralization. In this paper, the sequence stratigraphic structure of the uranium-bearing series in Qianjiadian uranium deposit, southwest Songliao Basin, is studied based on seismic, well logging, core analysis and test data. The relationship between stratigraphic structure and uranium mineralization is discussed. It is found that the Yaojia Formation in Qianjiadian area is a complete third-order sequence. The bottom boundary of Yaojia Formation is a regional unconformity and the bottom part of Yaojia Formation is composed of mud conglomerate and sandstone with mud pebble. The top boundary of Yaojia Formation is a parallel unconformity, and the top part of Yaojia Formation comprise mauve mixed with gray mudstone. The initial flooding surface and the largest flooding surface have been recognized internally, which is divided into low system tract, transgressive system tract and high system tract. The low system tract distributes in a small area with an average thickness of about 40 meters, showing a long and narrow north-east distribution. The transgressive system tract and the high system tract continuously overlap, and the distribution area extends southwest to the Baxian Tube-Kailu County area, and the overall direction is still north-east. The average formation thickness in the study area is 85m and 75m respectively. The uranium mineralization of the Yaojia Formation in the study area is restrained by the sequence stratigraphic structure, and the uranium mineralization of the different small sequence groups from the bottom to the top gradually weakens in the vertical direction. On the plane, the distribution characteristics of uranium mineralization are different in different system tracts. The uranium mineralization in the low system tract mainly develops in the area of QianⅣ-QianⅤ.The ore bodies are plate-like and lenticular in shape, and are distributed in a north-east strike strip. Uranium mineralization in transgressive system tract in the Qian Ⅱ, Qian Ⅳ and Qian Ⅴ is irregular arc-shaped and the ore bodies are "roll-like", which is classical interlayer oxidation zone uranium mineralization. The uranium mineralization in high system tract mainly develops in Qian III and sporadic distribution in the south, and it is speculated that there is further prospecting space to the south. The study results can provide a basis for prospecting in the study area, and a basis for the study of uranium metallogenic model and process.
-
图 1 研究区构造位置及矿床分布图
Figure 1. Structural location and distribution map of ore deposits in the study area
图 2 钱家店地区姚家组层序地层综合图
Figure 2. Sequence and sedimentary composite histogram of Yaojia Formation in Qianjiadian
图 3 钱家店地区姚家组层序地层划分地震剖面(剖面位置见图 1)
SQ-K2qn.青山口组三级层序；SQ-K2y-LST.姚家组低位体系域；SQ-K2y-EST.姚家组湖扩体系域；SQ-K2y-HST.姚家组高位体系域；SQ-K2n.嫩江组三级层序
Figure 3. Sequence stratigraphic division of seismic section of Yaojia Formation in Qianjiadian area
图 4 钱Ⅳ-117-07井姚家组底界古风化壳和上覆冲刷面
Figure 4. Paleocrust-weathering and overlying scour surface of Yaojia Formation in Well QianⅣ-117-07
图 5 钱家店地区姚家组与嫩江组层序界面划分标志
①嫩江组深灰色泥岩；②嫩江组鲕粒灰岩；③姚家组紫红色泥岩, 含钙质结核；④姚家组浅红色泥岩；⑤姚家组灰色泥岩, 含炭化植物碎屑；⑥姚家组浅灰色泥岩
Figure 5. Sequence boundary dividing marks of Yaojia Formation and Nen River Formation in Qianjiadian area
图 6 钱家店地区姚家组三级层序内不同体系域的沉积面貌示意图
a.低位体系域；b.湖泊扩展体系域；c.高位体系域
Figure 6. Sedimentary features of different system tracts in the third-order sequence of Yaojia Formation in Qianjiadian area
图 7 钱家店地区姚家组层序地层格架下层间氧化带与铀矿化特征(剖面位置见图 1)
Figure 7. Characteristics of interlayer oxidation zone and uranium mineralization under sequence stratigraphic framework of Yaojia Formation in Qianjiadian area
表 1 钱家店地区姚家组主量元素特征
Table 1. Major element characteristics of Yaojia Formation in Qianjiadian area
样品编号 岩性 深度/
mw(U)/
10-6Na2O MgO Al2O3 SiO2 P2O5 K2O CaO TiO2 MnO TFe2O3 烧失量 CAI 地层单元 wB/% 09-05-01 浅灰色细砂岩 284.6 8.47 2.24 0.36 11.17 77.93 0.12 3.73 0.61 0.44 0.02 1.17 2.15 55.83 姚家组 09-05-04 浅灰色细砂岩 314.4 3.87 2.27 0.41 11.14 76.2 0.12 3.45 0.7 0.55 0.04 2.41 2.7 55.99 09-05-14 浅灰色细砂岩 405.5 3.11 1.96 0.36 9.94 79.32 0.13 3.28 0.68 0.33 0.03 1.68 2.19 55.35 09-05-18 浅灰色细砂岩 429.7 7.20 1.58 1.27 17.47 65.01 0.24 3.53 0.41 0.78 0.01 4.07 5.52 70.88 09-05-23 浅灰色细砂岩 445.4 2.49 2.01 0.16 9.99 80.74 0.14 3.24 0.19 0.28 0.01 1.47 1.75 58.2 青山口组 09-05-25 浅灰色细砂岩 466.3 14.30 2.29 0.49 11.22 76.67 0.11 3.65 0.66 0.32 0.05 1.90 2.63 55.69 09-05-30 浅灰色细砂岩 508.8 5.38 2.54 0.36 12.6 75.64 0.15 3.7 0.38 0.6 0.02 2.38 1.62 58.64 注：分析测试数据由中国地质大学(武汉)地质矿产与成矿过程国家重点实验室完成；U含量采用高纯锗能谱仪分析, 其他主量元素分析采用经典湿法化学分析方法测定(AxiosX射线光谱仪) 
下载: 导出CSV
表 2 钱家店铀矿床姚家组铀矿化信息统计
Table 2. Uranium mineralization information of the Yaojia Formation in Qianjiadian uranium deposit
层序单元 矿体层数 矿体厚度/m 矿体品位/10-6 平米铀量/(kg·m-2) 矿化面积/km2 铀资源量占比/% 矿化钻孔数/个 最大值 最小值 均值 最大值 最小值 均值 最大值 最小值 均值 最大值 最小值 均值 SQK2y-HST(Pss2) 9 1 1.8 5.6 0.1 1.06 137.3 52.8 75.4 1.89 0.01 0.20 10.11 0.32 49 SQK2y-HST(Pss1) 12 1 2.0 11.1 0.02 1.89 351.3 51.9 117.1 3.86 0.01 0.50 20.47 13.51 155 SQK2y-EST(Pss2) 25 2 4.2 45.3 0.15 5.03 564.9 55.8 113.5 20.37 0.01 0.82 52.36 14.26 286 SQK2y-EST(Pss1) 17 1 2.9 18.8 0.1 3.10 406.9 52.6 116.0 26.91 0.01 1.35 56.40 25.05 357 SQK2y-LST 16 1 2.8 26.8 0.1 3.13 341.2 51.1 107.5 24.79 0.01 1.56 59.06 46.85 404
下载: 导出CSV
表 3 钱家店铀矿床不同区块铀矿化信息对比
Table 3. Comparison of the uranium mineralization information in the different blocks of the Qianjiadian uranium deposit
层序地层单元(姚家组) 钱Ⅱ块 钱Ⅲ块 钱Ⅳ块 钱Ⅴ块 块段个数 平均品位/% 平均厚度/m 平均平米铀量/(kg·m-2) 资源量占比/% 块段个数 平均品位/% 平均厚度/m 平均平米铀量/(kg·m-2) 资源量占比/% 块段个数 平均品位/% 平均厚度/m 平均平米铀量/(kg·m-2) 资源量占比/% 块段个数 平均品位/% 平均厚度/m 平均平米铀量/(kg·m-2) 资源量占比/% HST(Pss2) 3 0.017 5.09 1.95 1.0 0 0 0 0 0.0 0 0 0 0 0.0 0 0 0 0 0.0 HST(Pss1) 9 0.032 8.48 4.68 13.4 15 0.024 5.6 2.86 98.8 3 0.041 2.96 2.55 0.2 1 0.014 3.6 1.06 1.6 EST(Pss2) 15 0.030 7.05 3.72 46.0 0 0 0 0 0.0 21 0.021 4.035 1.83 2.6 0 0 0 0 0.0 EST(Pss1) 7 0.037 9.23 5.52 39.6 0 0 0 0 0.0 98 0.026 4.46 2.45 31.0 3 0.024 2.12 1.33 15.8 LST 地层不发育 1 0.019 3.5 1.37 1.2 73 0.025 5.79 3.13 66.3 7 0.022 3.75 1.71 82.6
下载: 导出CSV
-
[1] 王正邦. 国外地浸砂岩型铀矿地质发展现状与展望[J]. 铀矿地质, 2002, 18(1): 9-21. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200201001.htmWang Z B. Current status and prospects of uranium geology developments of foreign in-situ leachable sandstone type uranium deposits[J]. Uranium Geology, 2002, 18(1): 9-21(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200201001.htm [2] 黄净白, 李胜祥. 试论我国古层间氧化带砂岩型铀矿床成矿特点、成矿模式及找矿前景[J]. 铀矿地质, 2007, 23(1): 7-15. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200701001.htmHuang J B, Li S X. Metallogenic characteristics, model and exploration prospect for the paleo-interlayer oxidation type sandstone-hosted uranium deposits in China[J]. Uranium Geology, 2007, 23(1): 7-15(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200701001.htm [3] 焦养泉, 吴立群, 荣辉, 等. 铀储层结构与成矿流场研究: 揭示东胜砂岩型铀矿床成矿机理的一把钥匙[J]. 地质科技情报, 2012, 31(5): 94-104. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205014.htmJiao Y Q, W L Q, Rong H, et al. Uranium reservoir architecture and ore-forming flow field study: A key of revealing Dongsheng sandstone type uranium deposit mineralization mechanism[J]. Geological Science and Technology Information, 2012, 31(5): 94-104(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205014.htm [4] 肖新建, 李子颖, 李胜祥. 层序地层学研究与砂岩型铀矿床找矿勘探[J]. 地质找矿论丛, 2003, 18(2): 84-87.Xiao X J, Li Z Y, Li S X. The sequence stratigraphy and the prospecting of sandstone type uranium deposit[J]. Resources Research, 2003, 2003, 18(2): 84-87(in Chinese with English abstract). [5] 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.htmJiao, 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(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501018.htm [6] 焦养泉, 吴立群, 荣辉. 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.htmJiao Y Q, Wu L Q, Rong H. 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(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201802009.htm [7] 权建平, 樊太亮, 焦养泉, 等. 层序结构对吐哈盆地SHT砂岩型铀矿成矿的控制作用[J]. 世界核地质科学, 2006, 23(3): 130-136. doi: 10.3969/j.issn.1672-0636.2006.03.002Quan J P, Fan T L, Jiao Y Q, et al. Control of sequence frameworks over mineralization in SHT sandstone-type uranium deposit[J]. World Nuclear Geoscience, 2006, 23(3): 130-136(in Chinese with English abstract). doi: 10.3969/j.issn.1672-0636.2006.03.002 [8] 郭庆银, 陈祖伊, 韩淑琴, 等. 层序地层学在砂岩型铀矿勘查中的应用现状与前景展望[J]. 铀矿地质, 2008, 24(1): 5-11. doi: 10.3969/j.issn.1000-0658.2008.01.002Guo Q Y, Chen Z Y, Han S Q, et al. Application status and vistas of sequence stratigraphy to the exploration of sandstone-hosted uranium deposits[J]. Uranium Geology, 2008, 24(1): 5-11(in Chinese with English abstract). doi: 10.3969/j.issn.1000-0658.2008.01.002 [9] 何忧, 荣辉, 黄琨, 等. 伊犁盆地水文地质条件与铀成矿的关系[J]. 地质科技通报, 2020, 39(5): 139-147. https://dzkjqb.cug.edu.cn/CN/abstract/abstract10059.shtmlHe Y, Rong H, Huang K, et al. Relationship between uranium mineralization and hydrologic condition in Yili Basin[J]. Bulletion of Geological Science and Technology, 2020, 39(5): 139-147(in Chinese with English abstract). https://dzkjqb.cug.edu.cn/CN/abstract/abstract10059.shtml [10] 邹才能, 薛叔浩, 赵文智, 等. 松辽盆地南部白垩系泉头组-嫩江组沉积层序特征与地层-岩性油气藏形成条件[J]. 石油勘探与开发, 2004, 31(2): 14-17. doi: 10.3321/j.issn:1000-0747.2004.02.003Zou C N, Xue S H, Zhao W Z. Depositional sequences and forming conditions of the Cretaceous stratigraphic-lithologic reservoirs in the Quantou-Nengjiang Formations, South Songliao Basin[J]. Petroleum Exploration and Development, 2004, 31(2): 14-17(in Chinese with English abstract). doi: 10.3321/j.issn:1000-0747.2004.02.003 [11] 高春云, 周立发. 鄂尔多斯盆地西缘南段若干不整合面特征及其构造意义[J]. 地质科技情报, 2019, 38(6): 121-132. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201906015.htmGao C Y, Zhao L f. Geological characteristics of unconformities and their tectonic significance in the southern section of western Ordos Basin[J]. Geological Science and Technology Information, 2019, 38(6): 121-132(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201906015.htm [12] 刘可行, 甘华军, 陈思, 等. 高精度层序格架下的陆相断陷湖盆沉积体系演化: 以南堡凹陷老爷庙地区东营组三段为例[J]. 地质科技情报, 2019, 38(3): 88-102. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903009.htmLiu K X, Gan H J, Chen S, et al. Evolution of sedomentary system of continental faulted lacustrine basin under high-precision sequence framework: A case from the third Member of Dongying Formation in Laoyemiao area, Nanpu Sag[J]. Geological Science and Technology Information, 2019, 38(3): 88-102(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201903009.htm [13] 刘洋. 东海盆地西湖凹陷沉积记录的天文旋回响应[J]. 地质科技通报, 2020, 39(2): 120-128. https://dzkjqb.cug.edu.cn/CN/abstract/abstract10029.shtmlLiu Y. Resoponse to astronomical forcing of sedimentary record in Xihu Depression, East China Sea Basin[J]. Bulletion of Geological Science and Technology, 2020, 39(3): 120-128(in Chinese with English abstract). https://dzkjqb.cug.edu.cn/CN/abstract/abstract10029.shtml [14] 赵岳, 邵龙义, 徐强, 等. 二连盆地乌兰察布坳陷南缘含铀岩系层序地层与铀成矿规律[J]. 矿业科学学报, 2018, 3(4): 323-334. https://www.cnki.com.cn/Article/CJFDTOTAL-KYKX201804002.htmZhao Y, Shao L Y, Xu Q, et al. Sequence stratigraphy and uranium mineralization model of uranium-bearing rock series in the southern margin of Erlian Basin[J]. Journal of Mining Science and Technology, 2018, 3(4): 323-334(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KYKX201804002.htm [15] 陈方鸿, 张明瑜. 钱家店凹陷赋铀岩系姚家组高分辨率层序地层学研究[J]. 铀矿地质, 2005, 21(3): 209-242. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200504003.htmChen F H, Zhang M Y. Study on high resolution sequence stratigraphy framework of uranium hosting rock series in Qianjiadian Sag[J]. Uranium Geology, 2005, 21(3), 209-242(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200504003.htm [16] 陈晓林, 向伟东, 李田港, 等. 松辽盆地QJD铀矿床层间氧化带的展布特征及其与沉积相、铀成矿的关系[J]. 世界核地质科学, 2006, 23(3): 137-144. doi: 10.3969/j.issn.1672-0636.2006.03.003Chen X L, Xiang W D, Li T G, et al. Distribution characteristics of inter layer oxidation zone and its relationship with sedimentary facies and uranium mineralization in QJD uranium deposit, Songliao Basin, NE China[J]. World Nuclear Geoscience, 2006, 23(3): 137-144(in Chinese with English abstract). doi: 10.3969/j.issn.1672-0636.2006.03.003 [17] 荣辉, 焦养泉, 吴立群, 等. 松辽盆地南部钱家店铀矿床后生蚀变作用及其对铀成矿的约束[J]. 地球科学, 2016, 41(1): 154-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201601013.htmRong H, Jiao Y Q, Wu L Q, et al. Epigenetic alteration and its constraints on uranium mineralization from the Qianjiadian uranium deposit, southern Songliao Basin[J]. Earth Science, 2016, 41(1): 154-164(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201601013.htm [18] 李建国, 金若时, 张博, 等. 松辽盆地西南部上白垩统姚家组原生黏土矿物组合特征及其找铀意义[J]. 地球学报, 2018, 39(3): 295-305. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201803004.htmLi J G, Jin R S, Zhang B, et al. Characteristics of primary clay minerals in the Upper Cretaceous Yaojia Formation of Southwest Songliao Basin and their significance[J]. Acta Geoscientia Sinica, 2018, 39(3): 295-305(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201803004.htm [19] Zhao L, Cai C F, Jin R S, et al. Mineralogical and geochemical evidence for biogenic and petroleum-related uranium mineralization in the Qianjiadian deposit, NE China[J]. Ore Geology Reviews, 2018, 101: 273-292. doi: 10.1016/j.oregeorev.2018.07.025 [20] Rong H, Jiao Y Q, Wu L Q, et al. Origin of the carbonaceous debris and its implication for mineralization within the Qianjiadian uranium deposit, southern Songliao Basin[J]. Ore Geology Reviews, 2019, 107: 336-352. doi: 10.1016/j.oregeorev.2019.02.036 [21] Rong H, Jiao Y Q, Liu X, et al. Effects of basic intrusions on REE mobility of sandstones and their geological significance: A case study from the Qianjiadian sandstone-hosted uranium deposit in the Songliao Basin[J]. Applied Geochemistry, 2020, 120: 104665. doi: 10.1016/j.apgeochem.2020.104665 [22] Jia J M, Rong H, Jiao Y Q, et al. Mineralogy and geochemistry of carbonate cement in sandstone and implications for mineralization of the Qianjiadian sandstone-hosted uranium deposit, southern Songliao Basin, China[J]. Ore Geology Reviews, 2020, 123: 103590. doi: 10.1016/j.oregeorev.2020.103590 [23] 董文明, 林锦荣, 夏毓亮, 等. 松辽盆15地西南部上白垩统层序地层特征与砂岩型铀成矿作用[J]. 世界核地质科学, 2007, 24(3): 125-135. https://www.cnki.com.cn/Article/CJFDTOTAL-GWYD200703003.htmDong W M, Lin J R, Xia Y L, et al. Sequence stratigraphy of the upper cretaceous and its relation to sandstone-type uranium mineralization in the southwest of Songliao Basin[J]. World Nuclear Geoscience, 2007, 24(3): 125-135(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GWYD200703003.htm [24] 孙钰, 钟建华, 姜在兴, 等. 松辽盆地南部坳陷期层序地层研究[J]. 中国石油大学学报: 自然科学版, 2006, 30(5): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200605000.htmSun Y, Zhong J H, Jiang Z X, et al. Study of sequence stratigraphy of depression period in southern Songliao Basin[J]. Journal of China University of Petroleum: Natural Science Edition, 2006, 30(5): 1-7(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200605000.htm [25] 卓弘春, 林春明, 李艳丽, 等. 松辽盆地北部上白垩统青山口-姚家组沉积相及层序地层界面特征[J]. 沉积学报, 2007, 25(1): 29-38. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200701003.htmZhuo H C, Lin C M, Li Y L, et al. Characteristics of sedimentary facies and sequence boundary in upper cretaceous Qingshankou-Yaojia Formation of northern Songliao Basin[J]. Acta Sedimentologica Sinica, 2007, 25(1): 29-38(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200701003.htm [26] 王树恒, 周华, 梁江平. 松辽盆地北部西斜坡姚家组分层特征及其成因分析[J]. 地层学杂志, 2008, 32(3): 327-332. doi: 10.3969/j.issn.0253-4959.2008.03.016Wang S H, Zhou H, Liang J P. The stratigraphic division and sedimentary genesis of the Yaojia Formation in the western slope region of the northern Songliao Basin[J]. Journal of Stratigraphy, 2008, 32(3): 327-332(in Chinese with English abstract). doi: 10.3969/j.issn.0253-4959.2008.03.016 [27] 程日辉, 王国栋, 王璞珺, 等. 松科1井南孔白垩系姚家组沉积序列精细描述: 岩石地层、沉积相与旋回地层[J]. 地学前缘, 2009, 16(2): 272-287. doi: 10.3321/j.issn:1005-2321.2009.02.021Cheng R H, Wang G D, Wang P J, et al. Description of Cretaceous sedimentary sequence of the Yaojia Formation recovered by CCSD S-Ⅰs borehole in Songliao Basin: Lithostratigraphy, sedimentary facies and cyclic stratigraphy[J]. Earth Science Frontiers, 2009, 16(2): 272-287(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2009.02.021 [28] 席党鹏, 李罡, 万晓樵, 等. 松辽盆地东南区姚家组-嫩江组一段地层特征与湖泊演变[J]. 古生物学报, 2009, 48(3): 556-568. doi: 10.3969/j.issn.0001-6616.2009.03.024Xi D P, Li G, Wan X Q, et al. Yaojia-lower Nenjiang formations and lake evolution of southeastern Songliao Basin, NE China[J]. Acta Palaeontologica Sinica, 2009, 48(3): 556-568(in Chinese with English abstract). doi: 10.3969/j.issn.0001-6616.2009.03.024 [29] 石兰婷, 潘树新, 郭维华, 等. 松辽盆地南部上白垩统中部组合层序界面的识别标志及高分辨率层序地层格架[J]. 沉积学报, 2010, 27(2): 235-242. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201002005.htmShi L T, Pan S X, Guo W, et al. Sequence boundary characteristics and its high resolution sequence stratigraphic framework of the middle oil-bearing beds in the South of Songliao Basin[J]. Acta Sedimentologica Sinica, 2010, 27(2): 235-242(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201002005.htm [30] 高玉友, 禹宝利, 于文斌, 等. 松辽盆地西南部钱家店-架玛吐地区姚家组铀成矿条件及控矿因素分析[J]. 世界核地质科学, 2008, 25(3): 150-156. https://www.cnki.com.cn/Article/CJFDTOTAL-GWYD200803009.htmGao Y Y, Yu B L, Yu W B, et al. Analysis on uranium metallogenic conditions and ore-controlling factors of Qianjiadian-Jiamatu area, southwest of Songliao Basin[J]. World Nuclear Geoscience, 2008, 25(3): 150-156(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GWYD200803009.htm [31] 马汉峰, 罗毅, 李子颖, 等. 松辽盆地南部姚家组沉积特征及铀成矿条件[J]. 铀矿地质, 2009, 25(3): 144-149. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200903002.htmMa H F, Luo Y, Li Z Y, et al. Sedimentary features and uranium metallogenic conditions of Yaojia Formation in southern Songliao Basin[J]. Uranium Geology, 2009, 25(3): 144-149(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ200903002.htm [32] 郑纪伟. 开鲁盆地钱家店铀矿床成矿地质条件及勘探潜力分析[J]. 铀矿地质, 2010, 26(4): 194-200. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ201004001.htmZheng J W. Geological setting and exploration potential of Qianjiadian uranium deposit in Kailu Basin[J]. Uranium Geology, 2010, 26(4): 194-200(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ201004001.htm [33] 宋鹰, 任建业, 欧阳怀忠, 等. 松辽盆地北部姚家组底界面特征及其动力学背景[J]. 石油学报, 2010, 31(2): 187-195. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201002004.htmSong Y, Ren J Y, Ouyang H Z, et al. Characteristics and dynamic background of bottom boundary in Yaojia Formation of the northern Songliao Basin[J]. Acta Petrolei Sinica, 2010, 31(2): 187-195(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201002004.htm [34] 郭巍, 刘招君, 董惠民. 松辽盆地层序地层特征及油气聚集规律[J]. 吉林大学学报: 地球科学版, 2004, 34(2): 216-221. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402010.htmGuo W, Liu Z J, Dong H M. The sequence stratigraphic features and hydrocarbon accumulation of Songliao Basin[J]. Journal of Jilin University: Earth Science Edition, 2004, 34(2): 216-221(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200402010.htm [35] 宋照亮, 刘丛强, 韩贵琳, 等. 乌江流域沉积岩风化过程中铀的富集与释放[J]. 环境科学, 2006, 27(11): 2273-2278. https://www.cnki.com.cn/Article/CJFDTOTAL-HJKZ200611023.htmSong Z L, Liu C Q, Han G L, et al. Enrichment and release of uranium during weathering of sedimentary rocks in Wujiang catchments[J]. Environmental Science, 2006, 27(11): 2273-2278(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HJKZ200611023.htm [36] 李朝阳, 刘玉平, 管太阳, 等. 不整合面中的成矿机制与找矿研究[J]. 地学前缘, 2004, 11(2): 353-360. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200402005.htmLi C Y, Liu Y P, Guan T Y, et al. Mineralization mechanism and prospection on unconformable contacts[J]. Earth Science Frontiers, 2004, 11(2): 353-360(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200402005.htm [37] 何中波. 沉积盆地不整合类型及其与砂岩型铀矿成矿的关系[J]. 铀矿地质, 2013, 29(3): 133-138. https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ201303004.htmHe Z B. Types of unconformity in sedimentary basin and its relation to sandstone hosted uranium mineralization[J]. Uranium Geology, 2013, 29(3): 133-138(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-YKDZ201303004.htm -
下载:
点击查看大图
图(7) / 表(3)
计量
- 文章访问数: 474
- PDF下载量: 523
- 被引次数: 0
