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有色金属(矿山部分):2025,77(2):-
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四川瓦多-龙古地区水系沉积物地球化学特征及其对找矿潜力和找矿方向的指示
徐云峰, 秦宇龙, 熊昌利, 廖芝华, 马志磊, 詹涵钰, 吴建亮
(四川省综合地质调查研究所)
Geochemical characteristics of stream sediments and implications for prospectivity prediction in the Wado-Longgu district, Sichuan Province
XU Yunfeng, QIN Yulong, XIONG Changli, LIAO Zhihua, MA Zhilei, Zhan Hanyu, Wu Jianliang
(Sichuan Institute of Comprehensive Geological Survey)
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投稿时间:2024-04-26    修订日期:2024-07-07
中文摘要: 四川瓦多-龙古地区大地构造位于松潘-甘孜造山带东部巴颜喀拉地块,成矿区带属于石渠-雅江Li-Be-Au-Pb-Zn-Sn成矿带内(Ⅳ-11)。目的:为了研究四川瓦多-龙古地区水系沉积物地球化学特征及其对找矿潜力和找矿方向的指示,。方法:本文在详细阐述区域成矿地质背景及地质特征基础上,系统分析了1∶5万水系沉积物测量Sn、W、Mo、Bi、Cu、Pb、Zn、Au、Ag、As、Sb、Hg、TFe、Co、Ni、Mn、Li、Be、Nb、Ta 、Rb、Cs、Sr等23个元素地球化学分布规律与组合特征。结果:研究区主要异常成矿元素为Li、Be,次要异常成矿元素为Pb、Zn、Au、Ag、W、Sn。Li-Be-Nb、Pb-Zn-Ag、Cu-As-Sb元素具有较好的组合相关性。Li-Be-Nb为稀散成矿元素,表现出伟晶岩的成矿专属性;Pb-Zn-Ag为亲硫成矿元素,在许多热液型硫化物矿床中共生。Au-Cu-As组合中,Au、Cu为中温元素,通常在斑岩型、矽卡岩型铜金矿中伴生产出,Cu多呈独立矿物产出,Au多赋存于铜矿物中,As为中温成矿元素,元素具较强的迁移能力,可作为金矿找矿指示元素。结论:以各个单元素组合好、与矿产或成矿地质体关系密切为指标,共圈定8个1∶5万水系沉积物主成矿元素组合异常,编号为AS-1、AS-2、AS-3、AS-4、AS-5、AS-6、AS-7、AS-8。结合成矿地质条件及已发现各类矿(床)点、矿化点,研究区可划分出稀有金属找矿区3个,铅锌银多金属矿找矿区3个,金多金属矿找矿区2个。其中最具找矿潜力的综合异常为AS-1与AS-6,具较好的花岗伟晶岩型锂(铍铌钽)矿找矿潜力,。意义:为在该地区进一步开展地质找矿工作指明了方向。
Abstract:The Waduo-Longgu area of Sichuan is geotectonically located in the Bayankala massif in the eastern part of the Songpan-Ganzi orogenic belt, and belongs to the Shiqu-Yajiang Li-Be-Au-Pb-Zn-Sn metallogenic belt (IV-11). Purpose: In order to discuss the implication of the stream sediments to the prospecting potential and direction in the Wado-Longgu district, Sichuan Province, . Method: we give detailed description of the regional metallogenic geological background and regional geological characteristics in this paper, based on which we systematically analyze the geochemical distribution characteristics of 23 elements of the 1:50000 stream sediments measurement of the Waduo-Longgu area, including Sn, W, Mo, Bi, Cu, Pb, Zn, Au, Ag, As, Sb, Hg, TFe, Co, Ni, Mn, Li, Be, Nb, Ta, Rb, Cs and Sr. Consequence: Li and Be are the main ore-forming elements,Pb, Zn, Au, Ag, W and Sn are the minor anomalous ore-forming elements in the area. Li-Be-Nb, Pb-Zn-Ag, Cu-As-Sb elements have good assemblage correlation, Li,Be and Nb are sparse ore-forming elements, showing the metallogenic specificity of pegmatite; Pb, Zn and Ag are sulphophile ore-forming elements, which coexist in many hydrothermal sulfide deposits. In Au-Cu-As assemblage, Au and Cu are intermediate-temperature elements, and often coexist in the porphyry-type and skarn-type Cu-Au deposits, in which Cu often occurs as independent mineral and Au exists in Cu mineral; As is an intermediate ore-forming element, with relatively strong migration ability, which can be regarded as indicating element for Au deposits. Conclusion: Based on the good combination of individual elements and the close relationship with minerals or metallogenic geological bodies, we delineate eight major ore-forming element assemblage anomalies of 1:50000 stream sediment measurements, including AS-1, AS-2, AS-3, AS-4, AS-5, AS-6, AS-7, AS-8; According to the metallogenic geological background and the discovered ore occurences or mineralization points, the study area can be divided into 3 rare metal prospecting areas, 3 lead-zinc-silver polymetallic ore prospecting areas, and 2 gold polymetallic ore prospecting areas. Among these areas, AS-1 and AS-6 comprehensive anomaly areas have the biggest potential to find granitic pegmatite-type lithium (beryllium-niobium-tantalum) mine. Significance: These anomalies pointed out the direction for further geological prospecting in the area.
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基金项目:国家重点研发计划(2022YFC2905001)、中国地质调查局12120113049500、121201004000150017-93)、四川省科技厅基金(2023NSFSC0267)和四川省地质调查研究院财政支持科研(SCIGS-CZDXM-2024003)项目联合资助。
引用文本:
徐云峰,秦宇龙,熊昌利,廖芝华,马志磊,詹涵钰,吴建亮.四川瓦多-龙古地区水系沉积物地球化学特征及其对找矿潜力和找矿方向的指示[J].有色金属(矿山部分),2025,77(2):.
XU Yunfeng,QIN Yulong,XIONG Changli,LIAO Zhihua,MA Zhilei,Zhan Hanyu,Wu Jianliang.Geochemical characteristics of stream sediments and implications for prospectivity prediction in the Wado-Longgu district, Sichuan Province[J].NONFERROUS METALS(Mining Section),2025,77(2):.

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