苏北原生金刚石找矿现存问题探讨

doi:10.19388/j.zgdzdc.2022.05.09

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Abstract The second round of diamond prospecting in Northern Jiangsu Province has lasted 8 years, without discovery of ore-bearing kimberlite or diamond deposits. Based on the actual prospecting in Northern Jiangsu and combined with the latest diamond ore-forming theory and advance, the authors in this paper put forward and discuss several issues restricting the prospecting of primary diamonds in Northern Jiangsu to further explore the prospecting direction. The results show the primary target of primary diamond prospecting in Northern Jiangsu Province is Paleozoic kimberlite, which is located in Western Tanlu fault zone. The kimberlite of this period may be covered under the nappe due to the existence of the Xusu arc structure. Although there is no genetic relationship between Tanlu fault zone and Paleozoic kimberlite rock, the rifted red basin controlled by its development in the extension stage may cause the Paleozoic kimberlite to be covered under the Cretaceous. The future prospecting direction should focus on the Chenggang uplift in the Tan-Lu fault zone, and the breccia-bearing basic rocks on the west side of the Tanlu fault zone are also worthy of attention. During the ore prospecting and exploration, the geological and topographical conditions of the work area, the adaptability and limitations should be fully considered to select the combination of exploration methods according to local conditions.

Key words： Northern Jiangsu Province primary diamond prospecting Kimberlite structure prospecting direction

Received: 06 November 2021

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	Articles by authors
	ZHANG Qi
	ZHOU Qizhong
	WANG Bo
	WANG Guoqiang
	FENG Xuezhi
	LUO Yue

Cite this article:

ZHANG Qi,ZHOU Qizhong,WANG Bo, et al. The discussion of primary diamonds exploration in Northern Jiangsu Province[J]. , 2022, 9(5): 79-88.

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http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2022.05.09 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2022/V9/I5/79

[1] 施建斌,周琦忠,张琪,等.苏北金刚石找矿简史及找矿方向探讨[J].华东地质,2017,38(S1):31-35.
Shi J B,Zhou Q Z,Zhang Q,et al.Brief history of diamond prospecting and discussion on prospecting direction in North Jiang-su[J].East China Geol,2017,38(S1):31-35.
[2] 周琦忠,施建斌,黄友波,等.江苏徐州西村金伯利岩管地质特征及其找矿意义[J].地质通报,2019,38(1):152-162.
Zhou Q Z,Shi J B,Huang Y B,et al.Geological characteristics and prospecting significance of Kimberlite pipe in Xicun area of Xuzhou,Jiangsu Province[J].Geol Bull China,2019,38(1):152-162.
[3] 黄友波,周琦忠,张琪,等.江苏徐州塔山橄榄玄武玢岩地球化学特征及其与金刚石成因关系[J].地质通报,2019,38(1):132-142.
Huang Y B,Zhou Q Z,Zhang Q,et al.Geochemical feature of olivine basaltic porphyrite in Tashan area of Xuzhou,Jiangsu Pro-vince,and its relation to diamond origin[J].Geol Bull China,2019,38(1):132-142.
[4] 周琦忠,张琪,冯学知,等.江苏徐州白露山岩管地质特征及与金刚石成因关系探讨[J].地质学报,2020,94(9):2748-2762.
Zhou Q Z,Zhang Q,Feng X Z,et al.Geological characteristics of the Bailushan rock mass and its relationship with diamond genesis in Xuzhou,Jiangsu Province[J].Acta Geol Sin,2020,94(9):2748-2762.
[5] 蔡逸涛,张洁,施建斌,等.华北克拉通南缘碱性基性岩金刚石成因探讨——来自红外光谱的证据[J].地质学报,2020,94(9):2736-2747.
Cai Y T,Zhang J,Shi J B,et al.A discussion on the origin of basite type diamonds in the southern part of North China Craton:Evidences from FTIR[J].Acta Geol Sin,2020,94(9):2736-2747.
[6] 周琦忠,张琪,冯学知,等.徐州睢宁白露山岩体中的铬铁矿化学成分及金刚石的含矿性研究[J].中国地质调查,2020,7(6):35-42.
Zhou Q Z,Zhang Q,Feng X Z,et al.Chemical composition of the chromite and diamond potentiality of Bailushan rock mass in Sui-ning area of Xuzhou[J].Geol Surv China,2020,7(6):35-42.
[7] 蔡逸涛,陈国光,张洁,等.安徽栏杆地区橄榄辉长岩地球化学特征及其与金刚石成矿的关系[J].资源调查与环境,2014,35(4):245-253.
Cai Y T,Chen G G,Zhang J,et al.Geochemical Features of the Olivine-gabbros and their Relationship with Diamond-mineralization in the Langan area,Anhui Province[J].Resour Surv Environ,2014,35(4):245-253.
[8] 路凤香,赵磊,邓晋福,等.华北地台金伯利岩岩浆活动时代讨论[J].岩石学报,1995,11(4):365-374.
Lu F X,Zhao L,Deng J F,et al.The discussion on the ages of kimberlitic magma activity in North China platform[J].Acta Pe-trol Sin,1995,11(4):365-374.
[9] 王登红,郑绵平,王成辉,等.大宗急缺矿产和战略性新兴产业矿产调查工程进展与主要成果[J].中国地质调查,2019,6(6):1-11.
Wang D H,Zheng M P,Wang C H,et al.Progresses and main achievements on bulk lacking minerals and strategic emerging industry minerals survey project[J].Geol Surv China,2019,6(6):1-11.
[10] 张培元. 论金刚石的成因和成矿作用及找矿方向[J].地质科技管理,1999,16(4):28-36.
Zhang P Y.The Discussion on the genesis,mineralization and prospecting direction of diamond[J].Geol Technol Manage,1999,16(4):28-36.
[11] 路凤香,郑建平,邵济安,等.华北东部中生代晚期—新生代软流圈上涌与岩石圈减薄[J].地学前缘,2006,13(2):86-92.
Lu F X,Zheng J P,Shao J A,et al.Asthenospheric upwelling and lithospheric thinning in late Cretaceous-Cenozoic in eastern North China[J].Earth Sci Front,2006,13(2):86-92.
[12] 郑建平,路凤香,O’Reilly S Y,等.华北地台东部古生代与新生代岩石圈地幔特征及其演化[J].地质学报,1999,73(1):47-56.
Zheng J P,Lu F X,O'Reilly S Y,et al.Comparison between palaeozoic and Cenozoic lithospheric mantle in the eastern part of the North China block:With a discussion of mantle evolution[J].Acta Geol Sin,1999,73(1):47-56.
[13] 牛漫兰. 郯庐断裂带中南段岩浆活动与深部过程[D].合肥:合肥工业大学,2001.
Niu M L.Magmatism and Deep Processes in the Central and Southern Segment of the Tanlu Fault Zone[D].Hefei:Hefei University of Technology,2001.
[14] Xu J W.The Tancheng-Lujiang Wrench Fault System[M].Chichester:John Wiley & Sons,Inc.,1993:1-7.
[15] Xu J W,Zhu G.Tetonic models of the Tan-Lu fault zone,eastern China[J].Int Geol Rev,1994,36(8):771-784.
[16] Yin A,Nie S Y.An indentation model for the North and South China collision and the development of the Tan-Lu and Honam fault systems,eastern Asia[J].Tectonics,1993,12(4):801-813.
[17] 徐学思. 初论郯庐断裂的平移及演化[J].中国区域地质,1985,6(4):37-42.
Xu X S.Horizontal displacement and evolution of the Tancheng-Lujiang fracture[J].Reg Geol China,1985,6(4):37-42.
[18] 宋瑞祥. 中国金刚石矿床专论——中国金刚石矿找矿与开发[M].北京:地质出版社,2013:12-225.
Song R X.Monograph on China’s Diamond Deposits[M].Beijing:Geological Publishing House,2013:12-225.
[19] 江苏省地质矿产局第五地质大队区调分队.(台儿庄幅(南1/2))I-50-56-A岔河幅I-50-56-B汴塘幅I-50-56-C邳城幅I-50-56-D八义集幅I-50-68-A邳县幅I-50-68-B双沟幅I-50-68-C古邳镇幅I-50-68-D 1∶5万区域地质调查报告(地质、矿产部分)[R].徐州:江苏省地矿局第5地质大队,1990.
NO.5 Geological Team of Jiangsu Geology and Mineral Bureau.1∶50 000 geological and mineral survey report of Taierzhuang Area(South 1/2),Chahe Area,Biantang Area,Picheng Area,Bayiji Area,Pixian Area,Shuanggou Area,Gupi Area[R].Xuzhou:NO.5 Geological Team of Jiangsu Geology and Mineral Bureau,1990.
[20] 周秀仲,黄蕴慧,秦淑英,等.山东、辽宁金伯利岩中石榴石的类型、标型特征及其与金刚石的关系[J].岩石矿物学杂志,1991,10(3):252-264.
Zhou X Z,Huang Y H,Qin S Y,et al.Types,Typomorphic characteristics of garnet from Kimberlites in Shandong and Liaoning province and its relationship with diamond[J].Acta Petrol Mineral,1991,10(3):252-264.
[21] 赵秀芳. 山东蒙阴县西峪矿区深部与外围金刚石指示矿物——利用金刚石指示矿物预测金伯利岩的含矿性[J].地质通报,2019,38(1):121-131.
Zhao X F.A study of diamond indicative minerals in the depth and periphery of Xiyu,Mengyin County,Shandong Province:Metallogenic properties of kimberlite predicted by diamond indicating minerals[J].Geol Bull China,2019,38(1):121-131.
[22] Dawson J B,Stephens W E.Statistical classification of garnets from Kimberlite and associated xenoliths[J].J Geol,1975,83(5):589-607.
[23] 张安棣. 金刚石找矿指示矿物研究及数据库[M].北京:北京科学技术出版社,1991:1-162.
Zhang A D.Diamond Prospecting Indicative Mineral Research and Database[M].Beijing:Beijing Science and Technology Press,1991:1-162.