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Radioactive geophysical features of Haizishan area in Litang of Sichuan Province |
CAO Yun, WANG Guanghui, MA Changwei, WANG Yongfei |
Sichuan Institute of Nuclear Geology, Chengdu 610052, China |
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Abstract In order to investigate the radioactive geophysical features, uranium metallogenetic geological setting and metallogenetic conditions at Haizishan area, the ground total gamma survey and geology-gamma spectrometric profile survey were conducted. The radioactive background of Haizishan area was preliminarily cognized through the ground total gamma survey and the radioactive features were identified. The anomaly properties of Late Yanshan granites were roughly confirmed through geology - gamma spectrometric profile survey, and the detailed statistical analysis was done for radionuclide contents of each major lithostratigraphy. The results show that Late Yanshan granites in this area have higher total gamma background value, and the distribution of total gamma anomaly is almost consistent with Late Yanshan granites. The uranium background value of the granites is higher, showing the uranium sources are favorable in this area. There is Chaqingka hot-spring anomaly in the western periphery of Haizishan area, which is in connection with the northwest fault. The sinter on the ground has very high total gamma measurement value, and the uranium - thorium anomaly occurrence is shown through gamma spectrometric survey. According to the geological and radiometric properties of Chaqingka hot-spring anomaly, combined with the uranium metallogenetic geological setting and metallogenetic conditions in the area, the authors identified that the potential source of uranium is bearing fluids containing uranium or the uranium is likely to be abundant in deep Late Yanshan granites. The uranium is migrated to deposit and enrich at the surface, which provides a prospecting target for further uranium exploration.
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Received: 11 November 2019
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[1] 张成江,周游.四川省海子山幅(H47E011015)1:5万水系沉积物化探测量报告[R].成都:成都理工大学,2015. [2] 李俊国. 四川省1:5万海子山幅水系沉积物地球化学特征及成矿潜力分析[D].成都:成都理工大学,2016. [3] 王江. 四川海子山地区水系沉积物铀钍地球化学特征[D].成都:成都理工大学,2017. [4] 李俊国,张成江,陈兴兵,等.海子山地区1:5万水系沉积物地球化学特征及钨、锡异常浅析[J].黑龙江冶金,2015,35(5):31-35. [5] 尹明辉. 川西海子山—格聂地区花岗岩岩石地球化学特征及铀成矿条件[D].成都:成都理工大学,2018. [6] 徐争启,张成江,周游,等.三江北段海子山地区铀钍地球化学异常特征及其找矿意义[J].物探化探计算技术,2016,38(6):837-842. [7] 陈兴兵,张成江,李俊国,等.四川甘孜海子山地区1:5万地球化学异常分析[J].矿物学报,2015,35(增刊1):567. [8] 李俊国,张成江,王江,等.义敦岛弧带海子山花岗岩体微量元素地球化学特征及成因分析[J].吉林大学学报(地球科学版),2015,45(增刊1):1510-15. [9] 边鹏. 义敦岛弧带成矿作用与成矿规律[D].成都:成都理工大学,2018. [10] 高雪. 义敦地体晚白垩世与侵入岩有关的多金属成矿作用[D].北京:中国地质大学(北京),2018. [11] 方小玉,彭头平,范蔚茗,等.义敦地块中—晚三叠世中酸性侵入岩起源及其地质意义探讨[J].地球化学,2017,46(5):413-434. [12] 方小玉. 义敦地块中—晚三叠世中酸性侵入岩:岩石成因及其地质意义探讨[D].广州:中国科学院大学(中国科学院广州地球化学研究所),2017. [13] 刘振. 四川省理塘地区图姆沟组火山岩岩石学特征及含矿性[D].成都:成都理工大学,2017. [14] 邹光富,毛英,毛琼,等.西南三江地区大地构造演化与成矿作用[J].矿物岩石,2017,37(1):15-29. [15] 宋婉婧. 川西晚白垩世岩浆活动的成因和驱动机制[D].北京:中国地质大学(北京),2019. [16] 侯增谦,莫宣学."三江"地区义敦岛弧的构造-岩浆演化特征[G]//李廷栋.青藏高原地质文集(21)——"三江"论文专辑.北京:地质出版社,1991:159-171. [17] 高永泰,李小壮,吴振林,等.1:20万区域地质调查报告(义敦幅H-47-XVI)[R].名山:四川省地质局区域地质调查队二分队,1980. [18] 李庆祥,文沛然,邓永福,等.1:5万义敦幅、海子山幅区域地质调查报告[R].成都:四川省地质矿产局区调队,1990. [19] 张方毅,赖绍聪,秦江锋.义敦岛弧带晚白垩世海子山二长花岗岩成因及其地质意义[J].高校地质学报,2018,24(3):340-352. [20] 王楠,吴才来,秦海鹏.川西义敦岛弧中生代典型花岗岩体矿物学、地球化学特征及岩浆来源探讨[J].地质论评,2017,63(4):981-1000. [21] 侯立玮,傅德明,肖懿.试用数学地质方法探讨川西义敦地区中酸性岩浆岩岩石化学特征、成岩成矿系列及演化[C]//地质矿产部青藏高原地质文集编委会.青藏高原地质文集(17)——地质矿产部青藏高原地质科学第二次讨论会论文集(二).北京:地质出版社,1985:335-353. [22] 周明海,胡泮芹,彭学顺,等.EJ/T 831—1994地面伽马总量测量规范[S].北京:中国核工业总公司,1994. [23] 于汇津,邓一谦.勘查地球物理概论[M].北京:地质出版社,1993:164-172. [24] 章晔,华荣洲,石柏慎,等.放射性方法勘查[M].北京:原子能出版社,1990:159-179. [25] 李正文,贺振华.勘查技术工程学[M].北京:地质出版社,2003:327-337. [26] 余水泉,马站军,朱捌,等.EJ/T 363—2012地面伽马能谱测量规范[S].北京:国家国防科技工业局,2013. [27] 李友良,颜启明,徐建张,等.EJ/T 1213—2006铀矿地质勘查成果分类分级[S].北京:国防科学技术工业委员会,2006. [28] 吴慧山. 核技术勘查[M].北京:原子能出版社,1998:68-76. [29] 李巨初,陈友良,张成江,等.铀矿地质与勘查简明教程[M].北京:地质出版社,2011:25-26. [30] 张万林. 铀矿地质简明教程[M].北京:原子能出版社,1987:32-33. |
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[2] |
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[3] |
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[4] |
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[5] |
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