宁芜、庐枞盆地玢岩铁矿成矿深度及成矿后抬升、剥蚀情况: 来自磷灰石裂变径迹的证据

刘文浩; 张均; 李婉婷; 孙腾; 江满容; 王健; 吴建阳; 陈曹军

doi:10.3799/dqkx.2012.105

Volume 37 Issue 5

Sep. 2012

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Article Navigation > Earth Science > 2012 > 37(5): 966-980

LIU Wen-hao, ZHANG Jun, LI Wan-ting, SUN Teng, JIANG Man-rong, WANG Jian, WU Jian-yang, CHEN Cao-jun, 2012. Metallogenic Depth, Post-Mineralization Uplift and Denudation of Porphyry-Like Type Iron Deposits in Ningwu, Luzong Basins: Evidences from Apatite Fission Track. Earth Science, 37(5): 966-980. doi: 10.3799/dqkx.2012.105

Citation:

LIU Wen-hao, ZHANG Jun, LI Wan-ting, SUN Teng, JIANG Man-rong, WANG Jian, WU Jian-yang, CHEN Cao-jun, 2012. Metallogenic Depth, Post-Mineralization Uplift and Denudation of Porphyry-Like Type Iron Deposits in Ningwu, Luzong Basins: Evidences from Apatite Fission Track. Earth Science, 37(5): 966-980. doi: 10.3799/dqkx.2012.105

Citation:

LIU Wen-hao, ZHANG Jun, LI Wan-ting, SUN Teng, JIANG Man-rong, WANG Jian, WU Jian-yang, CHEN Cao-jun, 2012. Metallogenic Depth, Post-Mineralization Uplift and Denudation of Porphyry-Like Type Iron Deposits in Ningwu, Luzong Basins: Evidences from Apatite Fission Track. Earth Science, 37(5): 966-980. doi: 10.3799/dqkx.2012.105

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Metallogenic Depth, Post-Mineralization Uplift and Denudation of Porphyry-Like Type Iron Deposits in Ningwu, Luzong Basins: Evidences from Apatite Fission Track

doi: 10.3799/dqkx.2012.105

Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2011-12-22
Available Online: 2021-11-10
Publish Date: 2012-09-15

Abstract

Abstract

The metallogenic depth and post-mineralization uplift and denudation are the key issues in deep prospecting, which have been weak in the study of mineral deposits due to the absence of effective technology. The authors select Dongshan, Meishan porphyry-like iron deposits in Ningwu basin and Nihe, Luohe porphyry-like iron deposits in Luzong basin formed about ~130 Ma as the study subjects for the metallogenic depth and post-mineralization uplift and denudation of porphyry-like iron deposits, with the help of AFT analysis of apatites in ore mineral assemblages. The results suggest: (1) the pooled AFT ages(1σ) of the four deposits are 106.3±5.4 Ma, 94.2±4.0 Ma, 81.3±4.0 Ma and 79.1±3.3 Ma, respectively, showing the ore bodies of four deposits passed the PAZ successively. The AFT ages and confined track lengths decrease with the increase of buried depth of samples and become close to the mineralization ages and the initial confined track length, which are possibly controlled by diverse uplift and denudation after mineralization leading to the different cooling rates while the samples passed the PAZ. (2) The thermal histories of AFT modeling reflect that there are two different cooling stages, namely the rapid cooling progress caused by losing of heat source and the slow cooling progress caused by uplift. The temperature inflection points between the two stages of the four deposits are probably identical, corresponding to a depth of 1.7 to 1.8 km. (3) Since 110 Ma, the uplift and denudation rate of the Ningwu basin have been greater than those of Luzong basin, so that most ore deposits in Ningwu basin buried shallowly or even exposed to the surface. The early uplift and denudation were controlled by the regional Yellow Bridge tectonic event.
- metallogenic depth,
- uplift,
- denudation,
- AFT,
- porphyry-like type iron deposit

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References(90)

References

Belton, D.X., Brown, R.W., Kohn, B.P., et al., 2004. Quantitative resolution of the debate over antiquity of the central Australian landscape: implications for the tectonic and geomorphic stability of cratonic interiors. Earth and Planetary Science Letters, 219(1-2): 21-34. doi: 10.1016/S0012-821X(03)00705-2

Bernet, M., Garver, J.I., 2005. Fission-track analysis of detrital zircon. In: Reiners, P.W., Ehlers, T.A., eds., Low-temperature thermochronology: techniques, interpretations, and applications. RIMG, 58: 205-238. doi: 10.2138/rmg.2005.58.8

Cao, X.Z., Sun, H.S., Xu, B.J., et al., 2008. Research on effective methods and approachs of rapid evaluation of potential concealed deposit(ore body) prospecting. China University of Geosciences Press, Wuhan, 26-30(in Chinese).

Carlson, W.D., Donelick, R.A., Ketcham, R.A., 1999. Variability of apatite fission-track annealing kinetics: I. Experimental results. American Mineralogist, 84(9): 1235-1255. doi: 10.2138/am-1999-0903

Chakurian, A.M., Arehart, G.B., Donelick, R.A., et al., 2003. Timing constraints of gold mineralization along the Carlin trend utilizing apatite fission-track, ⁴⁰Ar/³⁹Ar, and apatite (U-Th)/He methods. Economic Geology and the Bulletin of the Society of Economic Geologists, 98(6): 1159-1171. doi: 10.2113/gsecongeo.98.6.1159

Chen, B.L., 2001. Calculation of metallogenic depth of lode gold deposits from mineralization structure-dynamics. Chinese Journal of Geology, 36(3): 380-384(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX200103014.htm

Du, J.G., Chang, D.Y., 2011. Consideration on the deep-iron ore deposits prospecting in the middle-lower Yangtze metallogenic belt. Acta Geologica Sinica, 85(5): 687-698(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201105008.htm

Ehlers, T. A., Chaudhri, T., Kumar, S., et al., 2005. Computational tools for low-temperature thermochronometer interpretation. In: Reiners, P.W., Ehlers, T.A., eds., Low-temperature thermochronology: techniques, interpretations, and applications. RIMG, 58: 589-622. doi: 10.2138/rmg.2005.58.22

Fan, Y., Zhou, T.F., Yuan, F., et al., 2010. Geochronology of the diorite porphyrites in Ning-Wu basin and their metallogenic significances. Acta Petrologica Sinica, 26(9): 2715-2728(in Chinese with English abstract).

Fan, Y., Zhou, T.F., Yuan, F., et al., 2011. Geochronology of the porphyry-like type iron deposits in Ning-Wu basin: evidence from ⁴⁰Ar/³⁹Ar phlogopite dating. Acta Geologica Sinica, 85(5): 810-820(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201105017.htm

Fu, Q.P., McInnes, B.I.A., Davies, P.J., 2004. Numerical modelling of thermal and exhumation histories of magmatic ore deposits. Earth Science—Journal of China University of Geosciences, 29(5): 555-562(in Chinese with English abstract). http://www.researchgate.net/publication/291741121_Numerical_modeling_of_thermal_and_exhumation_histories_of_magmatic_ore_deposits

Gleadow, A.J.W., Duddy, I.R., Green, P.F., 1986. Confined fission-track lengths in apatite: a diagnostic-tool for thermal history analysis. Contributions to Mineralogy and Petrology, 94(4): 405-415. doi: 10.1007/BF00376334

Ketcham, R.A., Carter, A., Donelick, R.A., et al., 2007a. Improved measurement of fission-track annealing in apatite using c-axis projection. American Mineralogist, 92(5-6): 789-798. doi: 10.2138/am.2007.2280

Ketcham, R.A., Carter, A., Donelick, R.A., et al., 2007b. Improved modeling of fission-track annealing in apatite. American Mineralogist, 92(5-6): 799-810. doi: 10.2138/am.2007.2281

Li, X.M., Gong, W.J., Tan, K.X., et al., 2001. Preliminary discussion on the geological characteristics and mineralogenetic epoch of Xiaogela copper deposit in Lanping basin. Journal of East China Geological Institute, 24(1): 17-18(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HDDZ200101004.htm

Liu, D.M., Li, D.W., Yang, W.R., et al., 2005. Evidence from fission track ages for the tectonic uplift of the Himalayan orogen during Late Cenozoic. Earth Science—Journal of China University of Geosciences, 30(2): 147-152 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200502003.htm

Liu, Z.J., Wang, J.P., Zheng, D.W., et al., 2010. Exploration prospect and post-ore denudation in the northwestern Jiaodong gold province, China: evidence from apatite fission track thermochronology. Acta Petrologica Sinica, 26(12): 3597-3611 (in Chinese with English abstract).

Lu, H.Z., Fan, H.R., Ni, P., et al., 2004. Fluid inclusion. Science Press, Beijing, 230-240 (in Chinese).

Lv, G.X., Liu, R.X., Wang, F.Z., et al., 2000. A method for estimating the depth of petrogenesis and metallogenesis. Journal of Geomechanics, 6(3): 50-62 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLX200003005.htm

Ma, C.Q., Yang, K.G., Tang, Z.H., et al., 1994. Magma-dynamics of granitoids—theory, method and a case study of the eastern Hubei granitoids. China University of Geosciences Press, Wuhan, 60-70(in Chinese).

Ma, F., Jiang, S.Y., Xue, H.M., 2010. Early Cretaceous mineralizations Ningwu basin: insight from actinolite ³⁹Ar-⁴⁰Ar laser dating results. Mineral Deposits, 29(2): 283-289 (in Chinese with English abstract).

Maksaev, V., Munizaga, F., Zentilli, M., et al., 2009. Fission track thermochronology of Neogene plutons in the principal Andean Cordillera of central Chile (33-35 degrees S): implications for tectonic evolution and porphyry Cu-Mo mineralization. Andean Geology, 36(2): 153-171. doi: 10.5027/andgeoV36n2-a01

Marton, I., Moritz, R., Spikings, R., 2010. Application of low-temperature thermochronology to hydrothermal ore deposits: formation, preservation and exhumation of epithermal gold systems from the eastern Rhodopes, Bulgaria. Tectonophysics, 483(3-4): 240-254. doi: 10.1016/j.tecto.2009.10.020

McInnes, B.I.A., Evans, N.J., 2005. Application of thermochronology to hydrothermal ore deposits. Reviews in Mineralogy and Geochemistry, 58(1): 467-498. doi: 10.2138/rmg.2005.58.18

McInnes, B.I.A., Farley, K.A., Sillitoe, R.H., et al., 1999. Application of apatite (U-Th)/He thermochronometry to the determination of the sense and amount of vertical fault displacement at the Chuquicamata porphyry copper deposit, Chile. Economic Geology, 94(6): 937-947. doi: 10.2113/gsecongeo.94.6.937

Mei, L.F., Liu, Z.Q., Tang, J.G., et al., 2010. Mesozoic intra-continental progressive deformation in western Hunan-Hubei-eastern Sichuan provinces of China: evidence from apatite fission track and balanced cross-section. Earth Science—Journal of China University of Geosciences, 35(2): 161-174 (in Chinese with English abstract). doi: 10.3799/dqkx.2010.017

Ning-Wu Research Project Writing Team, 1978. Porphyry-like type iron deposits in Ning-Wu basin. Geological Publishing House, Beijing, 87-162(in Chinese).

Qin, Y.J., Zeng, J.N., Zeng, Y., et al., 2010. Zircon LA-ICP-MS U-Pb dating of ore-bearing pyroxene-trachyandesite porphyry and its geological significance in Luohe-Nihe iron ore field in Luzong basin, southern Anhui, China. Geological Bulletin of China, 29(6): 851-862(in Chinese with English abstract).

Reiners, P.W., Ehlers, T.A., Zeitler, P.K., 2005. Past, present, and future of thermochronology. In: Reiners, P.W., Ehlers, T.A., eds., Low-temperature thermochronology: techniques, interpretations, and applications. RIMG, 58: 1-18. doi: 10.2138/rmg.2005.58.1

Shen, C.B., Mei, L.F., Fan, Y.F., et al., 2005. Advances and prospects of apatite fission track thermochronology. Geological Science and Technology Information, 24(2): 57-63(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200502014.htm

Shen, C.B., Mei, L.F., Xu, Z.P., et al., 2007. Fission track thermochronology evidence for Mesozoic-Cenozoic uplifting of Daba Mountain, central China. Acta Petrologica Sinica, 23(11): 2901-2910 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200711021.htm

Shen, C.B., Mei, L.F., Xu, S.H., 2009. Fission track dating of mesozoic sandstones and its tectonic significance in the eastern Sichuan basin, China. Radiation Measurements, 44(9-10): 945-949. doi: 10.1016/j.radmeas.2009.10.001

Shi, X.B., Qiu, X.L., Liu, H.L., et al., 2006. Cenozoic cooling history of Lingcang granitoid batholith, western Yunnan: evidence from fission track data. Chinese Journal of Geophysics, 49(1): 135-142 (in Chinese with English abstract). doi: 10.1002/cjg2.820/full

Skinner, B.J., 1997. Hydrothermal mineral deposits: what we do and don't know. In: Barnes, H.L., ed., Geochemistry of hydrothermal ore deposits(third edition). John Wiley & Sons, Inc., New York, 1-30.

Sun, F.Y., Jin, W., Li, B.L., et al., 2000. Consideration about mineralization depth of lode gold deposits. Journal of Changchun University of Science and Technology, 30: 27-30(in Chinese with English abstract).

Tang, Y.C., Wu, Y.C., Chu, G.Z., et al., 1998. Geology of copper-gold polymetallic deposits in the along-Changjiang area of Anhui Province. Geological Publishing House, Beijing, 45-85(in Chinese).

Tang, Y.H., Yuan, W.M., Han, C.M., et al., 2003. Fission track age of the Yuerya gold deposit. Acta Geoscientica Sinica, 24(6): 573-578(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB200306018.htm

Wang, J.P., Zhai, Y.S., Liu, J.J., et al., 2008. A new approach to post-ore change and preservation of ore deposits: fission track analysis. Advances in Earth Science, 23(4): 421-427(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200804012.htm

Wanger, G.A., Haute, V.D.P., 1992. Fission-track dating. Kulwer Academic Publishers, Dordrecht.

Wei, J.X., 1984. Characters of fluid inclusions and mechanism of mineralization alterations for the volcanic deposits in the Lujiang-Zongyang basin. Bulletin of the Institute of Mineral Deposits, Chinese Academy of Geological Sciences, 1: 40-56(in Chinese with English abstract). http://www.researchgate.net/publication/284581384_Characters_of_fluid_inclusions_and_mechanism_of_mineralization_alterations_for_the_volcanic_deposits_in_the_Lujiang-Zongyang_basin

Xu, C.H., Zhou, Z.Y., Chang, Y., et al., 2010. Genesis of Daba arcuate structural belt related to adjacent basement: constraints from fission-track and (U-Th)/He thermochronology. Sci. China (Series D), 40(12): 1684-1696(in Chinese with English abstract).

Xu, X.T., Yuan, W.M., Gong, Q.J., et al., 2010. The analysis of zircon fission track's ore-forming epoch in Shaquanzi copper-iron deposits, Xinjiang. China Mining Magazine, 19(4): 105-108(in Chinese with English abstract). http://www.researchgate.net/publication/284971002_The_analysis_of_zircon_fission_track's_ore-forming_epoch_in_Shaquanzi_copper-iron_deposits_Xinjiang

Yuan, W.M., Wang, S.C., Wang, L.F., 2000. Metallogenic thermal history of the Wulonggou gold deposits in East Kunlun Mountains in the light of fission track thermochronology. Acta Geoscientia Sinica, 21 (4): 389-395(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/dqxb200004008

Yuan, W.M., Wang, S.C., Wang, L.F., 2001. Apatite and zircon fission track study on the mineralization age and its thermal history of Nanliang gold deposits, eastern Hebei, China. Acta Mineralogica Scinica, 21(2): 225-230(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWXB200102020.htm

Yu, J.J., Mao, J.W., 2002. ⁴⁰Ar-³⁹Ar albite dating and significance of the Porphyry-like type iron deposits in Ning-Wu basin. Progress in Natural Science, 12(10): 1059-1063 (in Chinese with English abstract).

Zhai, Y.S., Deng, J., Peng, R.M., 2000. Research contents and methods for post-ore changes, modifications and preservation. Earth Science—Journal of China University of Geosciences, 25(4): 340-345 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DQKX200004001.htm

Zhai, Y.S., Deng, J., Wang, J.P., et al., 2004. Researches on deep ore prospecting. Mineral Deposits, 23(2): 142-149(in Chinese with English abstract). http://www.researchgate.net/publication/292798938_Researches_on_deep_ore_prospecting

Zhang, D.H., Zhou, S.H., Wan, T.F., et al., 2007. Depth of ore deposit formation and prognosis deep-seated ore deposits. Geological Bulletin of China, 26(12): 1509-1518(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200712002.htm

Zhang, D.H., Xu, J.H., Yu, X.Q., et al., 2011. The diagenetic and metallogenic depth: main constraints and the estimation methods. Geological Bulletin of China, 30(1): 112-125(in Chinese with English abstract). http://www.researchgate.net/publication/281080318_The_diagenetic_and_metallogenic_depth_main_constriants_and_the_estimation_methods

Zhang, P., Zhou, Z.Y., Xu, C.H., 2009. Thermo-tectonic history of the Lower Yangtze area since Late Cretaceous: evidence from apatite fission track analysis of sandstones from Pukou Formation. Offshore Oil, 29(4): 26-32 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HYSY200904006.htm

Zhang, Y.H., 1991. Huangqiao transform event in tectonic evolution of Lower Yangtze region and the Meso-Paleozoic hydrocarbon exploration target. Oil & Gas Geology, 12(4): 439-448(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT199104009.htm

Zhao, W.G., Wu, M.A., Zhang, Y.Y., et al., 2011. Geological Characteristics and genesis of the Nihe Fe-S deposit, Lujiang Country, Anhui Province. Acta Geologica Sinica, 85(5): 789-801(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201105015.htm

Zhou, T.F., Fan, Y., Yuan, F., et al., 2011. Petrogensis and metallogeny study of the volcanic basins in the middle and Lower Yangtze metallogenic belt. Acta Geologica Sinica, 85(5): 712-730(in Chinese with English abstract). http://www.researchgate.net/publication/285443329_Petrogensis_and_metallogeny_study_of_the_volcanic_basins_in_the_Middle_and_Lower_Yangtze_metallogenic_belt

曹新志, 孙华山, 徐伯俊, 等, 2008. 隐伏矿床(体)找矿前景快速评价的有效方法与途径研究. 武汉: 中国地质大学出版社, 26-30.

陈柏林, 2001. 从成矿构造动力学探讨脉状金矿床成矿深度. 地质科学, 36(3): 380-384. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200103014.htm

杜建国, 常丹燕, 2011. 长江中下游成矿带深部铁矿找矿的思考. 地质学报, 85(5): 687-698. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201105008.htm

范裕, 周涛发, 袁峰, 等, 2010. 宁芜盆地闪长玢岩的形成时代及对成矿的指示意义. 岩石学报. 26(9): 2715-2728. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201009017.htm

范裕, 周涛发, 袁峰, 等, 2011. 宁芜盆地玢岩型铁矿床的成矿时代: 金云母⁴⁰Ar-³⁹Ar同位素年代学研究. 地质学报, 85(5): 810-820. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201105017.htm

傅清平, McInnes, B.I.A., Davies, P.J., 2004. 岩浆成矿体系的热演化和剥露史的数字模拟. 地球科学——中国地质大学学报, 29(5): 555-562. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405008.htm

李小明, 龚文君, 谭凯旋, 等, 2001. 兰坪盆地小格拉铜矿床地质特征及成矿时代初探. 华东地质学院学报, 24(1): 17-18. doi: 10.3969/j.issn.1674-3504.2001.01.005

刘德明, 李德威, 杨巍然, 等, 2005. 喜马拉雅造山带晚新生代构造隆升的裂变径迹证据. 地球科学——中国地质大学学报, 30(2): 147-152. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200502003.htm

柳振江, 王建平, 郑德文, 等, 2010. 胶东西北部金矿剥蚀程度及找矿潜力和方向——来自磷灰石裂变径迹热年代学的证据. 岩石学报, 26(12): 3597-3611. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201012013.htm

卢焕章, 范宏瑞, 倪培, 等, 2004. 流体包裹体. 北京: 科学出版社, 230-240.

吕古贤, 刘瑞珣, 王方正, 等, 2000. 成岩成矿深度构造校正测算和实测. 地质力学学报, 6(3): 50-62. doi: 10.3969/j.issn.1006-6616.2000.03.006

马昌前, 杨坤光, 唐仲华, 等, 1994. 花岗岩类岩浆动力学: 理论方法及鄂东南花岗岩类例析. 武汉: 中国地质大学出版社, 60-70.

马芳, 蒋少湧, 薛怀民, 2010. 宁芜盆地凹山和东山铁矿床中阳起石的激光³⁹Ar-⁴⁰Ar年代学研究. 矿床地质, 29(2): 283-289. doi: 10.3969/j.issn.0258-7106.2010.02.009

梅廉夫, 刘昭茜, 汤济广, 等, 2010. 湘鄂西-川东中生代陆内递进扩展变形: 来自裂变径迹和平衡剖面的证据. 地球科学——中国地质大学学报, 35(2): 161-174. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201002000.htm

宁芜研究项目编写小组, 1978. 宁芜玢岩铁矿. 北京: 地质出版社, 87-162.

覃永军, 曾键年, 曾勇, 等, 2010. 安徽南部庐枞盆地罗河-泥河铁矿田含矿辉石粗安玢岩锆石LA-ICP-MS U-Pb定年及其地质意义. 地质通报, 29(6): 851-862. doi: 10.3969/j.issn.1671-2552.2010.06.007

沈传波, 梅廉夫, 凡元芳, 等, 2005. 磷灰石裂变径迹热年代学研究的进展与展望. 地质科技情报, 24(2): 57-63. doi: 10.3969/j.issn.1000-7849.2005.02.011

沈传波, 梅廉夫, 徐振平, 等, 2007. 大巴山中-新生代隆升的裂变径迹证据. 岩石学报, 23(11): 2901-2910. doi: 10.3969/j.issn.1000-0569.2007.11.020

施小斌, 丘学林, 刘海龄, 等, 2006. 滇西临沧花岗岩基新生代剥蚀冷却的裂变径迹证据. 地球物理学报, 49(1): 135-142. doi: 10.3321/j.issn:0001-5733.2006.01.019

孙丰月, 金巍, 李碧乐, 等, 2000. 关于脉状热液金矿床成矿深度的思考. 长春科技大学学报, 30(增刊): 27-30.

唐永成, 吴言昌, 储国证, 等, 1998. 安徽沿江地区铜多金属矿床地质. 北京: 地质出版社, 45-85.

汤云晖, 袁万明, 韩春明, 等, 2003. 峪耳崖金矿的成矿时代裂变径迹研究. 地球学报, 24(6): 573-578. doi: 10.3321/j.issn:1006-3021.2003.06.018

王建平, 翟裕生, 刘家军, 等, 2008. 矿床变化与保存研究的裂变径迹新途径. 地球科学进展, 23(4): 421-427. doi: 10.3321/j.issn:1001-8166.2008.04.012

魏佳秀, 1984. 卢枞盆地火山岩矿床流体包裹体研究及矿化蚀变机理. 中国地质科学院矿床地质研究所所刊, 1: 40-56. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198400009006.htm

徐长海, 周祖翼, 常远, 等, 2010. 大巴山弧形构造带形成与两侧隆起的关系: FT和(U-Th)/He低温热年代约束. 中国科学: 地球科学, 40(12): 1684-1696. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201012006.htm

徐晓彤, 袁万明, 龚庆杰, 等, 2010. 利用裂变径迹定年分析新疆沙泉子铜铁矿成矿时代. 中国矿业, 19(4): 105-108. doi: 10.3969/j.issn.1004-4051.2010.04.030

袁万明, 王世成, 王兰芬, 2000. 东昆仑五龙沟金矿床成矿热历史的裂变径迹热年代学证据. 地球学报, 21 (4): 389-395. doi: 10.3321/j.issn:1006-3021.2000.04.008

袁万明, 王世成, 王兰芬, 2001. 裂变径迹分析法研究河北南梁金矿床成矿时代及其热历史. 矿物学报, 21(2): 225-230. doi: 10.3321/j.issn:1000-4734.2001.02.020

余金杰, 毛景文, 2002. 宁芜玢岩铁矿钠长石⁴⁰Ar-³⁹Ar定年及意义. 自然科学进展, 2(10): 1059-1063. doi: 10.3321/j.issn:1002-008X.2002.10.010

翟裕生, 邓军, 彭润民, 2000. 矿床变化与保存的研究内容和研究方法. 地球科学——中国地质大学学报, 25(4): 340-345. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200004001.htm

翟裕生, 邓军, 王建平, 等, 2004. 深部找矿研究问题. 矿床地质, 23(2): 142-149. doi: 10.3969/j.issn.0258-7106.2004.02.003

张德会, 周圣华, 万天丰, 等, 2007. 矿床形成深度与深部成矿预测. 地质通报, 26(12): 1509-1518. doi: 10.3969/j.issn.1671-2552.2007.12.002

张德会, 徐九华, 余心起, 等, 2011. 成岩成矿深度: 主要影响因素与压力估算方法. 地质通报, (1): 112-125. doi: 10.3969/j.issn.1671-2552.2011.01.012

张沛, 周祖翼, 许长海, 2009. 苏皖下扬子区晚白垩世以来的构造-热历史: 浦口组砂岩磷灰石裂变径迹证据. 海洋石油, 29(4): 26-32. doi: 10.3969/j.issn.1008-2336.2009.04.026

张永鸿, 1991. 下扬子区构造演化中的黄桥转换事件与中、古生界油气勘探方向. 石油与天然气地质, 12(4): 439-448. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT199104009.htm

赵文广, 吴明安, 张宜勇, 等, 2011. 安徽省庐江县泥河铁硫矿床地质特征及成因初步分析. 地质学报. 85(5): 789-801. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201105015.htm

周涛发, 范裕, 袁峰, 等, 2011. 长江中下游成矿带火山岩盆地的成岩成矿作用. 地质学报, 85(5): 712-730. doi: 10.3969/j.issn.1004-9665.2011.05.011

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Metallogenic Depth, Post-Mineralization Uplift and Denudation of Porphyry-Like Type Iron Deposits in Ningwu, Luzong Basins: Evidences from Apatite Fission Track

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