| China Geological Survey Chinese Academy of Geological Sciences | Host |
| 科学出版社 | Publish |
| Citation: |
ZHOU Hongzhi, XU Chongwen, ZHANG Songtao, ZHANG Libin, ZHANG Xinming. 2019. The 1:100 000 Mineralogical Dataset of the Gouli Gold Deposit Integrated Exploration Area in Dulan County, Qinghai Province[J]. Geology in China, 46(S1): 93-104. doi: 10.12029/gc2019Z111
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The 1:100 000 Mineralogical Dataset of the Gouli Gold Deposit Integrated Exploration Area in Dulan County, Qinghai Province
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Abstract
The 1:100 000 mineralogical dataset of the Gouli Gold Deposit integrated exploration area in Dulan County, Qinghai Province (also referred to as "the Area") consists of a systematic database, tectonic formation maps, mineralogical maps, geomagnetic ΔT plane isoline maps, geomagnetic ΔT RTP plane isoline maps, geochemical integrated anomalies maps, mineral prediction result maps, and attached tables. In the folder of each map, there are the corresponding preparation manuals for the map. The Area is divided into four second-order tectonic units by the Central Suture Zone of the East Kunlun Orogenic Belt from the Neoproterozoic Era to the Early Paleozoic Era (from Pt3 to the end of P2), the Xinghai-Kuhai Suture Zone from the Middle Paleozoic Era to the Late Paleozoic Era (from D to P3), and the A'nyemaqen Suture Zone from the Late Paleozoic Era to the Early Mesozoic Era (from C to the end of T2). The magmatic activities in the Area mainly occurred from the Ordovician to the Devonian and from the Permian to the Triassic, which represents two different orogenic cycles. The metallogenic period may be from the Late Triassic Epoch to the Early Jurassic Epoch. A total of 21 magnetic anomalies and 80 geochemical integrated anomalies on a scale of 1:50 000 were delineated in the Area. Furthermore, four grade Ⅲ metallogenic belts (areas), seven grade IV metallogenic sub-belts, eight grade V metallogenic belts (ore fields), and 17 grade VI favorable prospecting blocks were determined. 14 prospecting target areas were screened and submitted in the favorable prospecting blocks. In addition, a number of mineral deposits (occurrences) with prospecting potential were found in the Area through follow-up work, such as the Nagenkangqieer large-scale silver deposit, the Delong gold deposit, the Mailong gold occurrence, the Langmuri copper-nickel occurrence, and the Longshigeng copper-cobalt occurrence. It is estimated that the total amount of gold, silver, lead-zinc and copper-cobalt resources in the Area are 588.04 tons, 3 197.85 tons, 2 358 300 tons, and 1 214 900 tons respectively.
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References
[1] Chen Jiajie, Wei Junhao, Fu Lebing, Li Huan, Zhou Hongzhi, Zhao Xu, Zhan Xiaofei, Tan Jun. 2017. Multiple sources of the Early Mesozoic Gouli batholith, Eastern Kunlun Orogenic Belt, northern Tibetan Plateau: Linking continental crustal growth with oceanic subduction[J]. Lithos, 292−293: 161−178. doi: 10.1016/j.lithos.2017.09.006 [2] Liu Yongshen, Hu Zhaochu, Zong Keqing, Gao Changgui, Gao Shan, Xu Juan, Chen Haihong. 2010. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 55(15): 1535−1546. doi: 10.1007/s11434-010-3052-4 [3] Ludwig KR. 2012.User's manual for Isoplot 3.75—A geochronological toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center Special Publication No. 5, 1−75. [4] Xia Rui, Wang Changming, Qing Min, Li Wenliang, Emmanuel John M. Carranza, Guo Xiaodong, Ge Liangsheng, Zeng Guanzhong. 2015. Zircon U-Pb Dating, Geochemistry and Sr-Nd-Pb-Hf-O Isotopes for the Nan'getan granodiorites and mafic microgranular enclaves in the East Kunlun Orogen: Record of closure of the Paleo-Tethys[J]. Lithos, 234−235, : 47−60. [5] 陈加杰, 付乐兵, 魏俊浩, 田宁, 熊乐, 赵玉京, 张玉洁, 祁月清. 2016. 东昆仑沟里地区晚奥陶世花岗闪长岩地球化学特征及其对原特提斯洋演化的制约[J]. 地球科学, 41(11): 1863−1882. [6] 丰成友, 张德全, 李大新, 佘宏全. 2003. 青海东昆仑造山型金矿硫、铅同位素地球化学[J]. 地球学报, 24(6): 593−598. doi: 10.3321/j.issn:1006-3021.2003.06.022 [7] 蒋敬业, 程建萍, 祁士华, 向武. 2006. 应用地球化学[M]. 武汉: 中国地质大学出版社, 147−148. [8] 李碧乐, 沈鑫, 陈广俊, 杨延乾, 李永胜. 2012. 青海东昆仑阿斯哈金矿Ⅰ号脉成矿流体地球化学特征和矿床成因[J]. 吉林大学学报(地球科学版), 42(6): 1676−1687. [9] 李华健, 王庆飞, 杨林, 于华之, 王璇. 2017. 青藏高原碰撞造山背景造山型金矿床:构造背景、地质及地球化学特征[J]. 岩石学报, 33(7): 2189−2201. [10] 刘大文. 2004. 区域地球化学数据的归一化处理及应用[J]. 物探与化探, 28(3): 273−275. doi: 10.3969/j.issn.1000-8918.2004.03.024 [11] 刘颜, 付乐兵, 王凤林, 魏俊浩, 管波, 谭俊, 杨宝荣, 汪殿钟. 2018. 东昆仑东段坑得弄舍多金属矿床Pb-Zn与Au-Ag成矿关系研究[J]. 大地构造与成矿学, 42(3): 480−493. [12] 马昌前, 熊富浩, 尹烁, 王连训, 高珂. 2015. 造山带岩浆作用的强度和旋回性: 以东昆仑古特提斯花岗岩类岩基为例[J]. 岩石学报, 31(12): 3555−3568. [13] 潘彤. 2004. 青海东昆仑督冷沟铜钴矿床控矿条件的探讨[J]. 矿产与地质, 18(2): 109−112. doi: 10.3969/j.issn.1001-5663.2004.02.004 [14] 唐洋, 付乐兵, 杨宝荣, 祁月清, 谢智勇, 李文君, 马忠贤. 2017. 东昆仑东段果洛龙洼脉状金矿床断裂构造控矿规律[J]. 地质科技情报, 36(2): 160−167. [15] 岳维好, 高建国, 周家喜. 2013. 青海果洛龙洼金矿基性岩脉锆石U-Pb年龄及岩石地球化学特征[J]. 矿物岩石, 33(3): 93−102. doi: 10.3969/j.issn.1001-6872.2013.03.014 [16] 张雪亭, 杨生德, 杨站君. 2007. 青海省板块构造研究:100万青海省大地构造图说明书[M]. 北京: 地质出版社, 1−220. [1] Chen Jiajie, Fu Lebing, Wei Junhao, Tian Ning, Xiong Le, Zhao Yujing, Zhang Yujie, Qi Yueqing. 2016. Geochemical characteristics of late ordovician granodiorite in Gouli Area, eastern Kunlun orogenic belt, Qinghai Province: Implications on the evolution of Proto-Tethys ocean[J]. Earth Science, 41(11): 1863−1882 (in Chinese with English abstract). [2] Chen Jiajie, Wei Junhao, Fu Lebing, Li Huan, Zhou Hongzhi, Zhao Xu, Zhan Xiaofei, Tan Jun. 2017. Multiple sources of the Early Mesozoic Gouli batholith, Eastern Kunlun Orogenic Belt, northern Tibetan Plateau: Linking continental crustal growth with oceanic subduction[J]. Lithos, 292-293: 161−178. doi: 10.1016/j.lithos.2017.09.006 [3] Feng Chengyou, Zhang Dequan, Li Daxin, She Hongquan. 2003. Sulfur and lead isotope geochemistry of the orogenic gold deposits in east Kunlun area, Qinghai Province[J]. Earth Science, (06): 593−598 (in Chinese with English abstract). doi: 10.3321/j.issn:1000-2383.2003.06.002 [4] Jiang Jingye, Cheng Jianping, Qi Shihua, Xiang Wu. 2006. Applied Geochemistry [M]. Wuhan: China university of Geosciences Press, 147−148 (in Chinese). [5] Li Bile, Shen Xin, Chen Guangjun, Yang Yanqian, Li Yongsheng. 2012. Geochemicl features of ore-forming fluids and metallogenesis of veinⅠ in Asiha gold deposit, eastern Kunlun, Qinghai, Province[J]. Journal of Jilin University (Earth Science Edition), 42(06): 1676−1687 (in Chinese with English abstract). [6] Li Huajian, Wang Qingfei, Yang Lin, Yu Huazhi, Wang Xuan. 2017. Orogenic gold deposits formed in Tibetan collisional orogen setting: Geotectonic setting, geological and geochemical features[J]. Acta Petrologica Sinica, 33(7): 2189−2201 (in Chinese with English abstract). [7] Liu Dawen. 2004. The normalization of regional geochemical data and its application[J]. Geophysical and Geochemical Exploration, 28(3): 273−275, 279 (in Chinese with English abstract). doi: 10.3969/j.issn.1000-8918.2004.03.024 [8] Liu Yan, Fu Lebing, Wang Fenglin, Wei Junhao, Guan Bo, Tan Jun, Yang Baorong, Wang Dianzhong. 2018. Relationship Between Pb-Zn and Au-Ag Mineralization of Kengdenongshe Polymetallic Deposit in Eastern Segment of the Eastern Kunlun[J]. Geotectonica et Metallogenia, 42(03): 480−493 (in Chinese with English abstract). [9] Liu Yongshen, Hu Zhaochu, Zong Keqing, Gao Changgui, Gao Shan, Xu Juan, Chen Haihong. 2010. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 55(15): 1535−1546. doi: 10.1007/s11434-010-3052-4 [10] Ludwig K R. 2012. User's manual for Isoplot 3.75—A geochronological toolkit for Microsoft Excel [M]. Berkeley: Berkeley Geochronology Center Special Publication No. 5, 1 − 75. [11] Ma Changqian, Xiong Fuhao, Yin Shuo, Wang Lianxun, Gao Ke. 2015. Intensity and cyclicity of orogenic magmatism: An example from a Paleo-Tethyan granitoid batholith, Eastern Kunlun, northern Qinghai-Tibetan Plateau[J]. Acta Petrologica Sinica, 31(12): 3555−3568 (in Chinese with English abstract). [12] Pan Tong. 2004. Discussion on ore controlling condition of Dulengou Cu-Co depoist in estern Kunlun metallogenic belt, Qinghai[J]. Mineral Resources and Geology, 18(02): 109−112 (in Chinese with English abstract). doi: 10.3969/j.issn.1001-5663.2004.02.004 [13] Tang Yang, Fu Lebing, Yang Baorong, Qi Yueqing, Xie Zhiyong, Li Wenjun, Ma Zhongxian. 2017. Ore controlling regularities of fault in the Guoluolongwa lode gold deposit,east segment of eastern Kunlun orogen[J]. Geological Science and Technology Information, 36(2): 160−167 (in Chinese with English abstract). [14] Xia Rui, Wang Changming, Qing Min, Li Wenliang, Emmanuel John M. Carranza, Guo Xiaodong, Ge Liangsheng, Zeng Guanzhong 2015. Zircon U-Pb Dating, Geochemistry and Sr-Nd-Pb-Hf-O Isotopes for the Nan'getan Granodiorites and Mafic Microgranular Enclaves in the East Kunlun Orogen: Record of Closure of the Paleo-Tethys[J]. Lithos, (234): 47−60. [15] Yue Weihao, Gao Jianguo, Zhou Jiaxi. 2013. LA-ICP-MS zicon U-Pb ages and lithogeochemistry of basic dykes in the guoluolongwa Au orefield, Qinghai Province, China[J]. Journal of Mineralogy and Petrology, 33(03): 93−102 (in Chinese with English abstract). doi: 10.3969/j.issn.1001-6872.2013.03.014 [16] Zhang Xueting, Yang Shengde, Yang Zhanjun. 2007. Instructions of 1︰1 000 000 Qinghai Tectonic Map in Study on Plate Tectonics of Qinghai Province.Beijing: Geological Publishing House, 1 − 220 (in Chinese). -
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ZHOU Hongzhi, XU Chongwen, ZHANG Songtao, ZHANG Libin, ZHANG Xinming. 2019. The 1:100 000 Mineralogical Dataset of the Gouli Gold Deposit Integrated Exploration Area in Dulan County, Qinghai Province[J]. Geology in China, 46(S1): 93-104. doi: 10.12029/gc2019Z111
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