GEOCHEMISTRY AND SEDIMENT PROVENANCE OF SANDSTONE FROM YAOJIA FORMATION IN CENTRAL DEPRESSION, SOUTHERN SONGLIAO BASIN
-
摘要:
沉积物源对研究含铀砂体展布和含铀流体运移通道均具有指示意义.以松辽盆地南部中央凹陷区姚家组为研究对象，在砂岩样品系统地球化学测试和收集邻区钱家店铀矿研究成果的基础上，讨论研究区姚家组砂岩的地球化学、形成环境和沉积物源并与钱家店地区对比.研究表明，姚家组砂岩碎屑相对富含硅和铝元素，岩石类型主要为岩屑砂岩和长石砂岩；稀土元素含量160.12×10-6~253.74×10-6，表现为轻稀土（La、Ce、Pr等）富集、重稀土（Ho、Er、Tm、Yb、Lu）平坦、中度铕（Eu）负异常；主量、微量和稀土元素揭示砂岩形成于干旱-半干旱气候，化学蚀变程度不高，物源构造背景为主动大陆边缘.结合区域构造背景，认为研究区与钱家店地区物源成分相似而物源的方向不同，研究区姚家组砂岩碎屑母质源自东北或西南物源，源岩类型主要为花岗闪长岩和花岗岩.
Abstract:The sediment provenance is of indicative significance to study the distribution of uranium sand body and migration channel of uranium fluid. Taking the Yaojia Formation in Central Depression of southern Songliao Basin as object, based on the systematic geochemical testing of sandstone samples and collected data of neighboring Qianjiadian uranium deposit, the paper discusses the geochemistry, formation environment and sediment provenance of sandstone of Yaojia Formation and compares with those in Qianjiadian area. The results show that the sandstone detrital of Yaojia Formation is relatively rich in Si and Al, with the main rock types of lithic sandstone and arkose. The REE content is 160.12×10-6-253.74×10-6, characterized by enriched LREEs (La, Ce, Pr, etc.), flat HREEs (Ho, Er, Tm, Yb and Lu) and moderate negative Eu anomaly. The analysis of major, trace and rare earth elements reveal that the sandstone was formed in arid-semiarid climate, without high degree of chemical alteration, and the tectonic setting of provenance is active continental margin. Combined with the regional tectonic background, it is considered that the provenance component of the study area is similar to that of Qianjiadian area, but the source directions are different. The parent material for sandstone detrital of Yaojia Formation in the study area is derived from the northeast or southwest provenance, with the main source rocks of granodiorite and granite.
-
Key words:
- petrogeochemistry /
- sediment provenance /
- Yaojia Formation /
- uranium deposit /
- Songliao Basin
-
-
表 1 研究区姚家组砂岩常量元素含量
Table 1. Major element contents in sandstone of Yaojia Formation in the study area
样品号 SiO2 Fe2O3 FeO Fe2O3T Al2O3 CaO MgO MnO Na2O K2O TiO2 P2O5 Y96-1 73.30 1.42 0.95 2.47 12.99 2.82 1.38 0.04 2.81 3.77 0.41 0.12 Y96-2 72.51 0.24 0.66 0.98 10.17 9.84 0.36 0.09 2.68 3.17 0.22 0.06 Y96-3 58.47 4.63 1.19 5.96 13.68 12.30 3.56 0.15 1.63 3.55 0.58 0.26 Y96-4 56.65 6.78 1.18 8.09 17.72 7.39 4.30 0.07 1.40 3.65 0.71 0.16 Y96-5 73.11 1.22 1.10 2.44 13.48 2.68 1.12 0.03 2.93 3.85 0.40 0.08 Y96-6 69.99 2.14 1.25 3.53 14.68 3.10 1.50 0.04 2.96 3.74 0.50 0.10 Y96-7 68.26 0.77 1.00 1.89 11.67 10.24 0.62 0.11 2.97 3.99 0.29 0.07 Y96-8 69.43 0.90 1.11 2.14 11.75 9.00 0.91 0.11 2.99 3.33 0.39 0.08 Y96-9 67.67 3.55 1.00 4.66 14.23 4.25 1.87 0.06 2.77 3.98 0.50 0.12 Y96-10 67.19 2.49 0.98 3.57 12.96 7.89 1.34 0.12 2.79 3.78 0.36 0.11 Y96-11 74.32 0.89 0.94 1.93 13.14 2.28 1.00 0.03 3.22 3.69 0.42 0.08 Y96-12 69.33 1.29 1.12 2.53 15.25 3.36 1.48 0.04 3.59 3.94 0.51 0.10 Y96-13 70.66 1.08 1.12 2.33 14.89 2.99 1.37 0.03 3.48 3.78 0.50 0.10 Y36-1 74.54 1.95 0.56 2.57 13.91 1.17 1.30 0.04 3.11 2.82 0.53 0.07 Y36-2 62.85 3.45 0.62 4.14 13.62 9.80 1.52 1.02 3.07 3.15 0.70 0.21 Y36-3 64.34 5.50 0.72 6.30 16.23 3.89 2.51 0.14 2.35 3.45 0.72 0.14 Y36-4 61.31 6.77 0.79 7.65 17.26 4.18 2.86 0.14 2.10 3.72 0.71 0.15 Y36-5 64.37 6.89 0.73 7.70 17.63 1.31 2.65 0.09 1.96 3.60 0.65 0.12 Y36-6 57.38 8.23 0.78 9.09 19.91 3.49 2.84 0.11 2.17 4.23 0.72 0.16 Y36-7 58.52 7.69 0.71 8.48 18.13 4.81 2.44 0.08 2.57 4.25 0.62 0.19 Y36-8 64.23 3.82 0.55 4.44 14.53 7.30 1.70 0.59 3.03 3.48 0.59 0.18 Y201-1 63.18 1.24 0.70 2.02 11.97 14.19 1.04 0.26 3.58 3.17 0.57 0.10 Y201-2 64.30 3.10 1.73 5.03 15.34 5.39 2.57 0.05 3.06 3.72 0.61 0.12 Y201-3 69.36 2.86 1.06 4.03 13.93 3.77 1.70 0.04 3.09 3.64 0.44 0.12 Y201-4 56.86 7.03 1.12 8.27 16.78 7.05 3.68 0.11 2.35 4.17 0.66 0.19 Y201-5 71.37 1.96 0.86 2.92 13.92 2.99 1.51 0.03 3.19 3.71 0.37 0.09 Y201-6 70.27 1.44 0.98 2.53 13.34 5.35 1.24 0.06 3.26 3.59 0.38 0.09 Y201-7 69.94 1.92 0.81 2.82 13.51 4.69 1.41 0.06 3.55 3.64 0.36 0.10 Y201-8 61.29 5.64 0.99 6.74 15.32 6.45 2.95 0.09 2.80 3.72 0.60 0.13 Y201-9 53.96 6.40 1.16 7.69 17.42 9.29 4.26 0.09 2.47 4.08 0.67 0.19 Y201-10 70.15 1.40 0.88 2.37 14.38 3.80 1.06 0.04 3.87 3.84 0.47 0.10 Y201-11 73.23 1.06 0.83 1.99 13.58 2.44 0.81 0.03 3.88 3.62 0.41 0.09 Y201-12 66.67 0.52 0.69 1.28 10.35 14.59 0.97 0.20 2.87 2.66 0.40 0.08 Y201-13 70.43 2.24 0.91 3.25 12.86 5.16 1.84 0.05 2.86 3.00 0.54 0.10 Y201-14 61.69 5.20 1.00 6.32 15.68 6.22 2.92 0.06 2.63 3.81 0.63 0.16 Y201-15 56.80 7.08 1.07 8.28 17.34 6.71 3.56 0.07 2.14 4.37 0.66 0.20 Y201-16 62.60 4.45 0.98 5.54 16.19 5.56 2.69 0.05 2.79 3.95 0.59 0.14 含量单位：%. 
下载: 导出CSV
表 2 研究区姚家组砂岩微量元素含量
Table 2. Trace element contents in sandstone of Yaojia Formation in the study area
样品号 Rb Sr Ba Th U Zr Hf Sc V Cr Co Zn Ni Y96-1 115.40 286.10 899.50 11.87 49.51 68.17 2.69 6.29 85.27 26.54 7.04 106.70 16.88 Y96-2 60.12 313.10 910.90 8.44 3.37 42.11 1.80 2.21 20.59 29.48 1.30 66.17 4.72 Y96-3 112.20 516.20 575.40 9.86 2.18 95.10 3.61 11.18 70.74 40.07 8.41 76.14 30.28 Y96-4 148.40 478.10 483.90 14.39 2.09 113.00 3.96 14.23 106.20 67.77 14.14 90.38 43.30 Y96-5 112.20 323.50 986.70 11.99 18.38 61.06 2.15 4.51 333.60 19.89 7.72 33.04 15.74 Y96-6 114.80 313.10 902.50 12.46 48.19 78.09 2.74 7.10 197.80 54.43 10.66 61.57 27.39 Y96-7 98.63 364.70 997.90 13.68 18.24 44.81 1.24 2.96 143.60 18.24 5.01 55.12 12.85 Y96-8 84.95 322.40 839.80 9.74 47.39 70.02 1.99 4.07 68.36 20.60 7.19 68.45 16.19 Y96-9 121.50 307.00 862.10 11.40 3.86 79.62 2.75 7.26 43.45 26.17 5.01 82.24 17.20 Y96-10 98.01 310.70 838.80 8.95 2.87 55.54 2.10 5.20 29.99 17.82 3.49 52.21 11.76 Y96-11 102.50 333.00 1016.00 13.67 7.56 61.54 2.31 4.35 53.74 17.98 3.30 41.22 8.29 Y96-12 114.80 368.20 1037.00 13.60 21.95 79.85 2.73 5.94 116.30 46.53 8.10 171.00 16.79 Y96-13 107.40 359.20 1008.00 18.69 20.02 80.75 2.95 5.88 94.19 26.61 5.59 88.03 13.66 Y36-1 94.95 275.90 536.80 10.84 2.26 89.48 3.13 6.63 82.46 20.27 8.08 87.29 14.79 Y36-2 101.40 315.60 1207.00 14.70 3.15 124.70 4.43 7.89 56.93 19.96 8.56 93.84 17.88 Y36-3 154.60 280.40 433.50 14.42 2.15 112.80 3.81 11.79 80.18 35.31 11.55 128.00 29.83 Y36-4 158.20 280.00 489.30 15.41 2.25 121.40 4.14 13.67 87.83 36.88 12.53 158.10 35.66 Y36-5 159.50 241.40 331.30 15.00 2.29 123.00 4.17 14.34 85.27 63.45 11.96 105.00 33.30 Y36-6 168.70 288.40 760.10 14.58 2.23 120.80 4.10 14.14 89.47 39.89 12.68 134.80 34.91 Y36-7 138.50 336.70 428.60 13.08 1.72 103.10 3.50 11.11 65.15 35.44 10.44 97.43 30.26 Y36-8 115.80 354.30 507.40 10.49 1.72 95.58 3.37 7.62 50.01 14.96 8.01 69.26 18.10 Y201-1 80.42 505.80 718.80 13.06 2.08 94.12 3.20 3.95 34.90 12.18 4.85 31.03 8.33 Y201-2 119.30 409.20 734.30 16.45 5.65 94.68 3.29 8.89 84.67 28.75 10.34 68.85 26.36 Y201-3 106.40 378.40 898.80 10.78 2.75 78.30 2.95 6.30 36.39 33.74 6.39 129.70 17.68 Y201-4 155.60 449.80 504.90 15.21 5.26 109.50 3.73 11.90 72.22 51.20 11.87 107.50 33.52 Y201-5 110.70 376.70 909.50 5.56 17.52 66.34 2.29 5.20 46.79 19.38 4.57 75.90 15.73 Y201-6 91.20 413.60 879.50 10.44 11.37 66.53 2.58 5.17 41.14 20.56 4.84 109.90 13.63 Y201-7 92.89 393.70 907.00 10.87 130.57 71.68 2.78 5.30 45.91 24.46 6.04 63.77 14.68 Y201-8 137.90 440.40 710.40 16.90 385.19 107.80 3.67 9.61 216.80 57.15 14.21 96.15 30.42 Y201-9 131.50 627.10 559.70 11.90 13.01 121.40 4.24 12.72 93.71 47.18 13.50 94.12 40.72 Y201-10 89.52 425.10 1029.00 13.78 3.15 76.74 2.63 4.20 34.76 25.81 3.95 41.61 11.55 Y201-11 93.86 407.30 1147.00 11.08 6.45 79.60 2.91 3.46 25.64 16.18 3.47 29.83 7.61 Y201-12 70.49 480.90 672.80 7.87 128.43 77.97 2.71 3.67 33.99 12.26 3.73 44.33 9.43 Y201-13 91.54 390.50 621.90 9.98 8.12 87.66 3.14 6.70 44.18 28.46 7.10 82.79 18.71 Y201-14 134.90 453.90 551.10 13.18 6.09 101.00 3.59 9.97 60.81 42.67 10.45 104.80 36.49 Y201-15 150.10 479.80 481.40 13.30 10.66 106.70 3.95 12.57 70.47 58.38 13.13 112.60 37.78 Y201-16 129.20 454.50 624.00 12.42 13.73 92.26 3.60 10.11 65.40 55.74 10.56 81.63 27.19 含量单位：10-6.
下载: 导出CSV
表 3 研究区姚家组砂岩稀土元素含量
Table 3. REE contents in sandstone of Yaojia Formation in the study area
样品号 La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu Y96-1 34.65 62.71 7.41 28.17 4.84 1.12 4.37 0.55 2.73 0.50 1.49 0.20 1.29 0.19 Y96-2 26.20 38.43 5.71 20.00 3.51 0.89 3.25 0.39 1.82 0.34 1.01 0.13 0.87 0.13 Y96-3 37.11 63.08 8.34 31.57 5.73 1.24 5.45 0.71 3.69 0.71 2.12 0.29 1.89 0.28 Y96-4 45.76 84.39 9.98 37.91 6.71 1.43 5.97 0.79 4.00 0.76 2.27 0.31 2.01 0.30 Y96-5 42.06 72.11 8.13 31.01 4.84 1.07 4.19 0.48 2.16 0.39 1.17 0.15 1.02 0.15 Y96-6 40.60 74.67 7.65 31.95 4.91 1.10 4.34 0.55 2.65 0.49 1.44 0.20 1.30 0.19 Y96-7 38.84 62.66 5.86 29.45 3.65 0.78 3.27 0.38 1.77 0.31 0.88 0.11 0.72 0.10 Y96-8 34.79 56.77 5.06 24.66 3.13 0.76 2.86 0.36 1.71 0.32 0.96 0.13 0.88 0.13 Y96-9 36.60 67.67 7.63 29.25 4.99 1.14 4.46 0.57 2.84 0.54 1.58 0.21 1.40 0.21 Y96-10 32.82 56.18 7.21 25.76 4.51 1.06 4.09 0.51 2.46 0.45 1.35 0.18 1.16 0.17 Y96-11 43.64 75.15 8.54 32.49 5.07 1.14 4.48 0.54 2.52 0.46 1.35 0.18 1.18 0.17 Y96-12 43.21 76.05 7.81 32.84 4.98 1.14 4.52 0.57 2.80 0.52 1.55 0.21 1.37 0.20 Y96-13 57.67 101.40 11.20 43.66 6.90 1.21 6.03 0.69 3.14 0.57 1.68 0.22 1.45 0.21 Y36-1 31.29 62.88 6.22 25.28 4.16 0.96 3.75 0.49 2.50 0.48 1.45 0.20 1.36 0.20 Y36-2 47.27 88.34 9.89 42.11 7.10 1.60 7.09 0.95 5.01 0.97 2.89 0.38 2.50 0.38 Y36-3 44.68 84.24 9.10 39.63 6.33 1.30 5.89 0.80 4.18 0.81 2.43 0.34 2.21 0.33 Y36-4 46.59 87.74 9.84 41.54 7.06 1.47 6.63 0.93 4.88 0.95 2.85 0.39 2.55 0.38 Y36-5 42.13 85.27 9.54 37.51 6.64 1.31 6.05 0.83 4.37 0.85 2.58 0.36 2.35 0.35 Y36-6 42.99 86.31 9.54 37.56 6.91 1.45 6.54 0.89 4.77 0.92 2.76 0.38 2.47 0.37 Y36-7 36.41 68.70 8.11 30.90 5.84 1.21 5.55 0.78 4.24 0.84 2.56 0.36 2.37 0.35 Y36-8 34.79 66.08 7.19 30.03 5.05 1.11 4.76 0.65 3.44 0.68 2.06 0.29 1.90 0.29 Y201-1 38.13 63.75 7.06 29.92 4.50 0.95 4.18 0.52 2.51 0.48 1.43 0.19 1.29 0.19 Y201-2 49.89 87.32 10.63 40.50 6.69 1.27 5.96 0.72 3.43 0.63 1.89 0.25 1.67 0.24 Y201-3 39.57 73.08 8.68 33.07 5.51 1.17 4.93 0.62 3.02 0.57 1.70 0.23 1.48 0.22 Y201-4 46.77 85.35 9.52 39.05 6.45 1.29 5.92 0.78 4.01 0.76 2.26 0.31 2.02 0.29 Y201-5 26.72 52.50 5.33 21.69 3.39 0.97 3.05 0.40 2.02 0.39 1.17 0.16 1.06 0.16 Y201-6 32.99 58.54 7.22 24.50 4.42 1.07 4.07 0.50 2.48 0.46 1.39 0.19 1.26 0.18 Y201-7 33.10 59.43 7.19 26.80 4.75 1.12 4.35 0.57 2.85 0.55 1.65 0.23 1.44 0.21 Y201-8 48.57 91.34 10.22 42.60 7.78 1.75 7.60 1.06 5.58 1.07 3.07 0.39 2.44 0.35 Y201-9 42.21 80.86 9.34 35.44 6.32 1.28 5.81 0.76 3.88 0.74 2.22 0.30 1.97 0.29 Y201-10 43.29 78.36 8.37 35.20 5.20 1.08 4.58 0.55 2.54 0.47 1.37 0.18 1.23 0.18 Y201-11 33.38 64.18 6.74 26.03 4.23 1.03 3.80 0.48 2.36 0.44 1.34 0.19 1.24 0.19 Y201-12 25.22 41.11 5.56 20.75 3.58 0.84 3.38 0.43 2.20 0.43 1.31 0.18 1.18 0.18 Y201-13 36.39 62.78 7.65 31.12 5.02 1.12 4.55 0.59 2.97 0.56 1.71 0.23 1.56 0.23 Y201-14 40.42 75.42 8.84 35.11 5.94 1.23 5.44 0.71 3.66 0.69 2.06 0.28 1.84 0.27 Y201-15 40.80 79.66 9.28 35.22 6.35 1.26 5.83 0.77 3.92 0.75 2.25 0.30 1.99 0.29 Y201-16 37.97 69.69 8.42 33.82 5.69 1.24 5.24 0.70 3.56 0.68 2.04 0.27 1.80 0.27 含量单位：10-6.
下载: 导出CSV
-
[1] 张森, 石蕾, 鞠楠, 等. "油铀兼探"的找矿思路在松辽盆地的应用——以中央拗陷区南部为例[J]. 地质与资源, 2018, 27(3): 257-262. doi: 10.3969/j.issn.1671-1947.2018.03.007 http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8463.shtml
Zhang S, Shi L, Ju N, et al. The "oil-uranium co-exploration" idea in Songliao Basin: A practice in southern Central Depression[J]. Geology and Resources, 2018, 27(3): 257-262. doi: 10.3969/j.issn.1671-1947.2018.03.007 http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract8463.shtml
[2] 万军, 陈振岩, 李清春, 等. 钱家店地区油铀成矿(藏)条件对比及综合勘探意义[J]. 中国石油勘探, 2020, 25(6): 13-25. doi: 10.3969/j.issn.1672-7703.2020.06.002
Wan J, Chen Z Y, Li Q C, et al. Comparative study on metallogenic conditions of uranium deposits and hydrocarbon accumulation conditions of oil reservoirs in the Qianjiadian area and its significance on comprehensive exploration[J]. China Petroleum Exploration, 2020, 25(6): 13-25. doi: 10.3969/j.issn.1672-7703.2020.06.002
[3] 苗培森, 陈印, 程银行, 等. 中国北方砂岩型铀矿深部探测新发现及其意义[J]. 大地构造与成矿学, 2020, 44(4): 561-575. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202004002.htm
Miao P S, Chen Y, Cheng Y H, et al. New deep exploration discoveries of sandstone-type uranium deposits in North China[J]. Geotectonica et Metallogenia, 2020, 44(4): 561-575. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202004002.htm
[4] 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. doi: 10.3969/j.issn.1000-0658.2009.03.003
Ma 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. doi: 10.3969/j.issn.1000-0658.2009.03.003
[5] 吴柏林, 张婉莹, 宋子升, 等. 鄂尔多斯盆地北部砂岩型铀矿铀矿物地质地球化学特征及其成因意义[J]. 地质学报, 2016, 90(12): 3393-3407. doi: 10.3969/j.issn.0001-5717.2016.12.009
Wu B L, Zhang W Y, Song Z S, et al. Geological and geochemical characteristics of uranium minerals in the sandstone-type uranium deposits in the north of Ordos Basin and their genetic significance[J]. Acta Geologica Sinica, 2016, 90(12): 3393-3407. doi: 10.3969/j.issn.0001-5717.2016.12.009
[6] 刘华健, 金若时, 李建国, 等. 松辽盆地北部含铀岩系沉积物源及铀源分析研究进展[J]. 地质调查与研究, 2017, 40(4): 281-289. doi: 10.3969/j.issn.1672-4135.2017.04.005
Liu H J, Jin R S, Li J G, et al. Advance in research for sedimentary and uranium source analysis of the uranium-bearing series in northern Songliao Basin[J]. Geological Survey and Research, 2017, 40(4): 281-289. doi: 10.3969/j.issn.1672-4135.2017.04.005
[7] 张天福, 张云, 金若时, 等. 鄂尔多斯盆地东北缘侏罗系层序界面特征对砂岩型铀矿成矿环境的制约[J]. 中国地质, 2020, 47(2): 278-299. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202002003.htm
Zhang T F, Zhang Y, Jin R S, et al. Characteristics of Jurassic sequence boundary surfaces on the northeastern margin of Ordos Basin and their constraints on the spatial-temporal properties of sandstone uranium mineralization[J]. Geology in China, 2020, 47(2): 278-299. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202002003.htm
[8] 陈方鸿, 张明瑜, 林畅松. 开鲁盆地钱家店凹陷含铀岩系姚家组沉积环境及其富铀意义[J]. 沉积与特提斯地质, 2005, 25(3): 74-79. doi: 10.3969/j.issn.1009-3850.2005.03.012
Chen F H, Zhang M Y, Lin C S. Sedimentary environments and uranium enrichment in the Yaojia Formation, Qianjiadian Depression, Kailu Basin, Nei Mongol[J]. Sedimentary Geology and Tethyan Geology, 2005, 25(3): 74-79. doi: 10.3969/j.issn.1009-3850.2005.03.012
[9] 罗毅, 何中波, 马汉峰, 等. 松辽盆地钱家店砂岩型铀矿成矿地质特征[J]. 矿床地质, 2012, 31(2): 391-400. doi: 10.3969/j.issn.0258-7106.2012.02.018
Luo Y, He Z B, Ma H F, et al. Metallogenic characteristics of Qianjiadian sandstone uranium deposit in Songliao Basin[J]. Mineral Deposits, 2012, 31(2): 391-400. doi: 10.3969/j.issn.0258-7106.2012.02.018
[10] 夏飞勇, 焦养泉, 荣辉, 等. 松辽盆地南部钱家店铀矿床姚家组砂岩地球化学特征及地质意义[J]. 地球科学, 2019, 44(12): 4235-4251. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201912034.htm
Xia F Y, Jiao Y Q, Rong H, et al. Geochemical characteristics and geological implications of sandstones from the Yaojia Formation in Qianjiadian uranium deposit, southern Songliao Basin[J]. Earth Science, 2019, 44(12): 4235-4251. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201912034.htm
[11] Blatt H, Middleton G, Murray R. Origin of sedimentary rocks[M]. New Jersey: Prentice-Hall, 1980.
[12] Herron M M. Geochemical classification of terrigenous sands and shales from core or log data[J]. Journal of Sedimentary Research, 1988, 58(5): 820-829.
[13] Suttner L J, Dutta P K. Alluvial sandstone composition and paleoclimate, Ⅰ: Framework mineralogy[J]. Journal of Sedimentary Research, 1986, 56(3): 329-345.
[14] 李浩, 陆建林, 左宗鑫, 等. 长岭断陷南部断陷层湖相优质烃源岩发育控制因素[J]. 石油与天然气地质, 2015, 36(2): 209-218, 229. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201502006.htm
Li H, Lu J L, Zuo Z X, et al. Controlling factors of high-quality lacustrine hydrocarbon source rocks in southern Changling Depression[J]. Oil & Gas Geology, 2015, 36(2): 209-218, 229. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201502006.htm
[15] Nesbitt H W, Young G M. Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J]. Geochimica et Cosmochimica Acta, 1984, 48(7): 1523-1534. doi: 10.1016/0016-7037(84)90408-3
[16] Roser B P, Korsch R J. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio[J]. The Journal of Geology, 1986, 94(5): 635-650. doi: 10.1086/629071
[17] Maynard J B, Valloni R, Yu H S. Composition of modern deep-sea sands from arc-related basins[C]//Leggett J K. Trench and Fore-arc Sedimentation. Geological Society, London, Special Publications, 1982, 10(1): 551-561.
[18] Floyd P A, Leveridge B E. Tectonic environment of the Devonian Gramscatho Basin, South Cornwall: Framework mode and geochemical evidence from turbiditic sandstones[J]. Journal of the Geological Society, 1987, 144(4): 531-542. doi: 10.1144/gsjgs.144.4.0531
[19] Floyd P A, Winchester J A, Park R G. Geochemistry and tectonic setting of Lewisian clastic metasediments from the Early Proterozoic Loch Maree Group of Gairloch, NW Scotland[J]. Precambrian Research, 1989, 45(1/3): 203-214. http://www.onacademic.com/detail/journal_1000035912470210_a168.html
[20] Bhatia M R. Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks: Provenance and tectonic control[J]. Sedimentary Geology, 1985, 45(1/2): 97-113. http://www.onacademic.com/detail/journal_1000033949482210_c714.html
[21] Gu X X, Liu J M, Zheng M H, et al. Provenance and tectonic setting of the Proterozoic turbidites in Hunan, South China: Geochemical evidence[J]. Journal of Sedimentary Research, 2002, 72(3): 393-407. http://www.onacademic.com/detail/journal_1000035912300110_d5c2.html
[22] 郭莹莹. 松辽盆地南部姚家组沉积体系分析[D]. 长春: 吉林大学, 2008: 36-46.
Guo Y Y. The analysis of the sedimentary system of Yaojia group in the south of Songliao Basin[D]. Changchun: Jilin University, 2008: 36-46.
[23] 王黎明, 刘长明, 席海银, 等. 松辽盆地南部协尔苏凹陷构造沉积演化与铀成矿关系[J]. 地质与资源, 2009, 18(4): 274-278. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract9339.shtml
Wang L M, Liu C M, Xi H Y, et al. The relationship between structural-sedimentary evolution and uranium mineralization in Xiersu Depression, southern Songliao Basin[J]. Geology and Resources, 2009, 18(4): 274-278. http://manu25.magtech.com.cn/Jweb_dzyzy/CN/abstract/abstract9339.shtml
[24] 白静, 徐兴友, 陈珊, 等. 松辽盆地长岭凹陷乾安地区青山口组一段沉积相特征与古环境恢复——以吉页油1井为例[J]. 中国地质, 2020, 47(1): 220-235. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202001019.htm
Bai J, Xu X Y, Chen S, et al. Sedimentary characteristics and paleo-environment restoration of the first member of Qingshankou Formation in Qian'an area, Changling Sag, Songliao Basin: A case study of Jiyeyou 1 Well[J]. Geology in China, 2020, 47(1): 220-235. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI202001019.htm
[25] 王天琪, 韩江涛, 侯贺晟, 等. 综合物探剖面揭示松辽盆地基底地质与地球物理特征——以过松科二井剖面为例[J]. 中国地质, 2019, 46(5): 1126-1136. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201905014.htm
Wang T Q, Han J T, Hou H S, et al. The utilization of integrated geophysical profiles to reveal the basement geology and geophysical characteristics of the Songliao Basin: A case study of the profile of Well SK-2[J]. Geology in China, 2019, 46(5): 1126-1136. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201905014.htm
-
图(7)
表(3)
计量
- 文章访问数: 904
- PDF下载数: 32
- 施引文献: 0