胶西北玲珑、焦家金矿田锆石(U-Th)/He年龄及其对成矿后剥露程度的指示

孙华山; 韩静波; 申玉科; 刘浏; 冷双良; 许冲; 杨巧梅; 葛风建; 欧阳淑冰; 邓旭

doi:10.3799/dqkx.2016.053

胶西北玲珑、焦家金矿田锆石(U-Th)/He年龄及其对成矿后剥露程度的指示

doi: 10.3799/dqkx.2016.053

1.
中国地质大学资源学院，湖北武汉 430074
2.
河北省地质矿产勘查开发局秦皇岛矿产水文工程地质大队，河北秦皇岛 066000
3.
中国地质科学院地质力学研究所，北京 100081
4.
广东省有色地质勘查院，广东广州 510080
5.
湖北省地质调查院，湖北武汉 430034
6.
河南省地质矿产勘查开发局第二地质勘查院，河南许昌 461000

基金项目:

中央高校基本科研业务费专项资金项目 CUG090102

国家自然科学基金项目 41172087

详细信息

作者简介:
孙华山(1969-)，男，副教授，主要从事成矿预测教学与科研工作. E-mail: sunhsh@cug.edu.cn

中图分类号: P62
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出版历程
- 收稿日期: 2015-06-29
- 刊出日期: 2016-04-15

Zircon (U-Th)/He Age and Its Implication for Post-Mineralization Exhumation Degree of Linglong and Jiaojia Goldfields, Northwest Jiaodong, China

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Qinhuangdao Team of Mineral hydrological Geology, Bureau of Geology and Exploration of Hebei Province, Qinhuangdao 066000, China
3.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
4.
Guangdong Nonferrous Metals Geological Exploration Institution, Guangzhou 510080, China
5.
Hubei Geological Survey, Wuhan 430034, China
6.
No.2 Geo-Exploration Institute, Henan Bureau of Geo-Exploration and Mineral Development, Xuchang 461000, China

摘要

摘要: 玲珑和焦家矿田是胶西北地区最负盛名的两个金矿田.目前有关这两个矿田成矿研究的成果已十分丰富，但是，成矿后隆升剥蚀程度的研究尚属空白.为此，利用最近兴起的低温热年代学技术，对两个矿田成矿后剥露程度进行了尝试研究.结果表明，玲珑矿田锆石(U-Th)/He年龄主要为80~100 Ma，焦家矿田锆石(U-Th)/He年龄主要为90~105 Ma.这些年龄与前人运用其他方法获得的成岩成矿年龄不同，其不是本区岩浆－热液成矿事件的年龄，而是成矿后花岗岩隆升剥蚀的热年龄.基于锆石(U-Th)/He年龄制约，估算本区成矿后隆升剥蚀速率大致与全球造山型金矿剥露速率相当(大约60 m/Ma).玲珑矿田总体比焦家矿田成矿后多剥露了600~900 m，焦家矿田深部找矿潜力应比玲珑矿田大.
- 锆石(U-Th)/He /
- 剥露程度 /
- 胶西北金矿集中区 /
- 矿产 /
- 矿床学
Abstract: The Linglong and Jiaojia goldfields are the two most famous goldfields in the Northwest Jiaodong with voluminous publication focused on gold mineralization. Whereas it is still a barren land as far to pay attention to the post-mineralization exhumation. Utilizing the latest low-temperature thermochronological technique, this work carries out a tentative research on the exhumation degree in the two goldfields. The results show that the zircon (U-Th)/He ages in Linglong goldfield vary predominantly between 80 and 100 Ma, while they are of significant concentration between 90 and 105 Ma in Jiaojia goldfield. These ages yielded in this work are different from those of the previous obtained by other methods, they are not the geochronological ages in respond to magmatic-hydrothermal mineralization events, instead they must have recorded the thermochronological ages of the post-mineralization exhumation of the granitoid rocks. Based on the constrain of the zircon (U-Th)/He ages, it can be concluded that the degree of exhumation in this area is roughly in agreement with that from the statistics of the global orogenic gold deposits, about 60 m/Ma. The amount of post-mineralization exhumation in the Linglong goldfield is overall ca. 600-900 m more than that in the Jiaojia goldfield, so the prospecting potential at deep part is larger in the Jiaojia goldfield than that in the Linglong goldfield.
- zircon (U-Th)/He /
- degree of exhumation /
- Northwest Jiaodong gold concentration area /
- mineral /
- ore deposit geology

HTML全文

图 1 玲珑矿田位置(a)和地质图(b)

据吕古贤和孔庆存(1993); 图中图例均为图b的图例

Fig. 1. Location (a) and geological sketch (b) of Linglong goldfield

下载: 全尺寸图片幻灯片

图 2 焦家矿田地质图

据孙华山等(2008)修编

Fig. 2. Geological sketch of Jiaojia goldfield

下载: 全尺寸图片幻灯片

图 3 玲珑(左)和焦家(右)金矿田钻孔取样位置、样品岩相学特征和各样品的ZHe加权平均年龄

Qtz.石英；Bt.黑云母；Ser.绢云母；Chl.绿泥石；Cb.方解石

Fig. 3. Sampling, petrology and the weighted average ages of ZHe for the Linglong (left) and Jiaojia (right) goldfields

下载: 全尺寸图片幻灯片

图 4 焦家矿田ZK4上部3个样品ZHe年龄－高程图解

Fig. 4. Age-elevation plot of the upper three samples from the borehole ZK4 in Jiaojia goldfield

下载: 全尺寸图片幻灯片

表 1 玲珑和焦家矿田花岗岩锆石(U-Th)/He测试结果

Table 1. The results of zircon (U-Th)/He dating for the Linglong and Jiaojia goldfields

矿田	样品	高程(m)	U(10^-6)	Th(10^-6)	Th/U	He(mL/min)	未校正年龄	2σ	F_t	校正年龄(Ma)	2σ
玲珑矿田	ZK14-2	-150.8	900	220	0.24	28.30	61.45	5.0	0.74	83.4	7.6
	ZK14-2	-150.8	1 290	323	0.25	27.40	70.67	5.4	0.71	99.9	8.8
	权重平均		--	--	--	--	65.70	3.8	--	90.6	5.8
	ZK14-4	-511.8	219	103	0.47	8.73	60.24	4.0	0.79	76.7	5.2
	ZK14-4		995	322	0.32	27.20	66.62	5.0	0.74	89.8	7.6
	ZK14-4		182	49	0.27	2.86	54.30	3.8	0.72	75.9	6.2
	权重平均		--	--	--	--	59.45	2.4	--	79.3	3.6
	ZK14-6	-966.8	340	153	0.45	7.53	63.85	4.0	0.73	88.0	6.4
	ZK14-6		421	119	0.28	6.60	59.12	3.8	0.71	83.3	6.2
	ZK14-6		619	135	0.22	11.70	60.80	4.6	0.72	84.1	7.2
	权重平均		--	--	--	--	61.22	2.4	--	85.2	3.8
	ZK14-8	-1 369.8	550	145	0.26	21.40	73.38	5.6	0.78	93.7	7.0
	ZK14-8		704	169	0.24	29.80	74.91	6.8	0.79	95.1	8.6
	ZK14-8		593	140	0.24	22.40	71.64	5.6	0.79	90.5	7.2
	权重平均		--	--	--	--	73.13	3.4	--	92.7	4.4
焦家矿田	ZK4-2	-315.8	1 062	241	0.23	10.60	70.28	6.4	0.69	102.3	10.2
	ZK4-2	-315.8	1 055	245	0.23	6.71	64.93	4.0	0.64	102.2	12.0
	权重平均		--	--	--	--	66.44	3.4	--	102.2	7.8
	ZK4-3	-505.8	1 292	130	0.10	54.90	84.65	7.2	0.76	112.0	10.4
	ZK4-3		541	93.3	0.17	16.40	80.83	6.2	0.74	109.9	9.6
	ZK4-3		831	109	0.13	11.70	59.34	4.8	0.69	85.4	7.6
	权重平均		--	--	--	--	67.21	3.8	--	99.1	5.2
	ZK4-4	-720.8	1 085	134	0.12	27.00	69.33	5.2	0.74	93.3	7.8
	ZK4-4		932	172	0.18	9.05	62.38	4.0	0.66	95.0	7.0
	ZK4-4		444	86	0.19	6.14	67.01	4.6	0.66	101.0	8.0
	权重平均		--	--	--	--	64.36	3.0	--	96.3	4.4
	ZK4-5	-970.8	2 225	177	0.08	23.40	51.94	4.0	0.66	78.4	6.8
	ZK4-5	-970.8	365	110	0.30	6.80	51.65	3.4	0.75	69.2	5.2
	权重平均		--	--	--	--	51.77	2.6	--	72.6	4.2
注：权重平均年龄=Y/X；其中，X=SUM(X₁, …, X_n), X_n为第n个样品测试误差平方的倒数.Y=SUM(Y₁, …, Y_n), Y_n为第n个样品测试年龄与X_n的乘积；权重平均误差为X平方根的倒数.

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参考文献(57)

Boyce, J.W., Hodges, K.V., Olszewski, W.J., et al., 2006.Laser Microprobe (U-Th)/He Geochronology.Geochimica et Cosmochimica Acta, 70(12):3031-3039.doi: 10.1016/j.gca.2006.03.019
Chang, Y., Wang, W., Zhou, Z.Y., 2010.Age-Elevation Relationship Method Limited by the Topographic Relief over the Sampling Transect.Chinese Journal of Geophysics, 53(8):1868-1874(in Chinese with English abstract). http://manu39.magtech.com.cn/Geophy/EN/abstract/abstract3233.shtml
Chen, G.Y., 1993.Genetic Mineralogy and Gold Mineralization of Guojialing Granodiorite in Jiaodong Region.China University of Geosciences Press, Wuhan, 131(in Chinese). doi: 10.1007/s00126-003-0368-x
Dodson, M.H., 1973.Closure Temperatures in Cooling Geological and Petrological System.Contributions Mineralogy Petrology, 40:259-274. doi: 10.1007/BF00373790
Ehlers, T.A., 2005.Crustal Thermal Processes and the Interpretation of Thermochronometer Data.Reviews in Mineralogy and Geochemistry, 58(1):315-350.doi: 10.2138/rmg.2005.58.12
Ehlers, T.A., Armstrong, P.A., Chapman, D.S., 2001.Normal Fault Thermal Regimes and the Interpretation of Low-Temperature Thermochronometers.Physics of the Earth and Planetary Interiors, 126(3):179-194.doi: 10.1016/S0031-9201(01)00254-0
England, P., Molnar, P., 1990.Surface Uplift, Uplift of Rocks, and Exhumation of Rocks.Geology, 18(12):1173-1177.doi:10.1130/0091-7613(1990)018＜1173:SUUORA＞2.3.CO; 2
Evans, N.J., Byrne, J.P., Keegan, J.T., et al., 2005.Determination of Uranium and Thorium in Zircon, Apatite, and Fluorite:Application to Laser (U-Th)/He Thermochronology.Journal of Analytical Chemistry, 60(12):1159-1165. doi: 10.1007/s10809-005-0260-1
Evans, N.J., Mcinnes, B.I.A., Mcdonald, B., et al., 2013.Emplacement Age and Thermal Footprint of the Diamondiferous Ellendale E9 Lamproite Pipe, Western Australia.Mineralium Deposita, 48(3):413-421.doi: 10.1007/s00126-012-0430-7
Fan, H.R., Zhai, M.G., Xie, Y.H., et al., 2003.Ore-Forming Fluids Associated with Granite-Hosted Gold Mineralization at the Sanshandao Deposit, Jiaodong Gold Province, China.Mineralium Deposita, 38:739-750. doi: 10.1007/s00126-003-0368-x
Farley, K.A., 2000.Helium Diffusion from Apatite:General Behavior as Illustrated by Durango Fluorapatite.Journal of Geophysical Research, 105(B2):2903-2914.doi: 10.1016/1999JB900348
Farley, K.A., Wolf, R.A., Silver, L.T., 1996.The Effects of Long Alpha-Stopping Distances on (U-Th)/He Ages.Geochimica et Cosmochimica Acta, 60(21):4223-4229.doi: 10.1016/S0016-7037(96)00193-7
Fu, F.Q., Mcinnes, B.I.A., Evans, N.J., et al., 2010.Numerical Modeling of Magmatic-Hydrothermal Systems Constrained by U-Th-Pb-He Time-Temperature Histories.Journal of Geochemical Exploration, 106(1):90-109. https://www.researchgate.net/profile/Brent_Mcinnes/publication/248533026_Numerical_modeling_of_magmatichydrothermal_systems_constrained_by_UThPbHe_timetemperature_histories/links/542ab66d0cf29bbc12688c37.pdf?disableCoverPage=true
Goldfarb, R., Santosh, M., 2013.The Dilemma of the Jiaodong Gold Deposits:Are They Unique? Geoscience Frontiers, 5(2):139-153.doi: 10.1016/j.gsf.2013.11.001
Harrison, T.M., Duncan, I., Mcdougall, I., 1985.Diffusion of ⁴⁰Ar in Biotite:Temperature, Pressure and Compositional Effects.Geochimica et Cosmochimica Acta, 49(11):2461-2468.doi: 10.1016/0016-7037(85)90246-7
Kesler, S.E., Wilkinson, B.H., 2006.The Role of Exhumation in the Temporal Distribution of Ore Deposits.Economic Geology, 101(5):919-922.doi: 10.2113/gsecongeo.104.5.623
Kesler, S.E., Wilkinson, B.H., 2009.Resources of Gold in Phanerozoic Epithermal Deposits.Economic Geology, 104(5):623-633.doi: 10.2113/gsecongeo.102.1.155
Lee, J.K., Williams, I.S., Ellis, D.J., 1997.Pb, U and Th Diffusion in Natural Zircon.Nature, 390(6656):159-162.doi: 10.1038/36554
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). https://www.researchgate.net/publication/282384011_Exploration_prospect_and_post-ore_denudation_in_the_northwestern_Jiaodong_Gold_Province_China_Evidence_from_apatite_fission_track_themochronology
Li, J.W., Vasconcelos, P.M., Zhang, J., et al., 2003.⁴⁰Ar/³⁹Ar Constraints on a Temporal Link between Gold Mineralization, Magmatism, and Continental Margin Transtension in the Jiaodong Gold Province, Eastern China.The Journal of Geology, 111(6):741-751.doi: 10.1086/378486
Lu, L.N., Fan, H.R., Hu, F.F., et al., 2011.Emplacement Depth of the Guojialing Granodiorites from the Northwestern Jiaodong Peninsula, Eastern China:Evidences from Hornblende Thermobarometry and Fluid Inclusions.Acta Petrologica Sinica, 27(5):1521-1532(in Chinese with English abstract). https://www.researchgate.net/publication/286880875_Emplacement_depth_of_the_Guojialing_granodiorites_from_the_Northwestern_Jiaodong_Peninsula_eastern_China_Evidences_from_hornblende_thermobarometry_and_fluid_inclusions
Lü, G.X., Kong, Q.C., 1993.Gold Deposit Geology Series:Gold Deposit of Linglong-Jiaojia Type in Jiaodong Peninsula.Science Press, Beijing, 253(in Chinese). http://www.sciencedirect.com/science/article/pii/S0169136814001541
Márton, 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, 483:240-254.doi: 10.1016/j.tecto.2009.10.020
McInnes, B.I.A., Evans, N.J., Fu, F.Q.et al., 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, 94:937-948.doi: 10.2113/gsecongeo.94.6.937
Miao, L.C., Luo, Z.K., Huang, J.Z., et al., 1997.Studies and Implication of Zicon SHRIMP of Granitic Intrusive in Zhaoye Metallogenic Belt, Shandong Province.Science in China(Series D), 27(3):207-213(in Chinese). doi: 10.1007/BF02879527
Qiu, Y.M., Groves, D.I., McNaughton, N.J., et al., 2002.Nature, Age, and Tectonic Setting of Granitoid-Hosted, Orogenic Gold Deposits of the Jiaodong Peninsula, Eastern North China Craton, China.Mineralium Deposita, 37(3-4):283-305. doi: 10.1007/s00126-001-0238-3
Qiu, Y.S., 1988.Regional Metallogenic Condition of Gold Deposits in the Zhaoyuan-Yexian District, Shandong Province, China.Liaoning Science and Technology Press, Shenyang, 268(in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX200001006.htm
Reiners, P.W., 2005.Zircon (U-Th)/He Thermochronometry.Reviews in Mineralogy and Geochemistry, 58(1):151-179. doi: 10.2138/rmg.2005.58.6
Reiners, P.W., Spell, T.L., Nicolescu, S., et al., 2004.Zircon (U-Th)/He Thermochronometry:He Diffusion and Comparisons with ⁴⁰Ar/³⁹Ar Dating.Geochimica et Cosmochimica Acta, 68(8):1857-1887. doi: 10.1016/j.gca.2003.10.021
Stockli, D.F., Farley, K.A., Dumitru, T.A., 2000.Calibration of the Apatite (U-Th)/He Thermochronometer on an Exhumed Fault Block, White Mountains, California.Geology, 28(11):983. doi: 10.1130/0091-7613(2000)28<983:COTAHT>2.0.CO;2
Sun, H.S., Sun, L., Cao, X.Z., et al., 2008.Axial Vertical Zoning Characteristics of Primary Halos and Geochemical Exploration Indicators for Deep Ore Body Prognosis in Shangzhuang Gold Deposit, Northwest Jiaodong Peninsula, Shangdong Province.Mineral Deposits, 27(1):64-70(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQHX201003002.htm
Wang, J.Y., Huang, S.P., 1990.Geothermic Dataset in Chinese Mainland.Seismology and Geology, 12(4):351-366(in Chinese). http://www.sciencedirect.com/science/article/pii/S1002007108001093
Wang, L.G., Qiu, Y.M., Mcnaughton, N.J., et al., 1998.Constraints on Crustal Evolution and Gold Metallogeny in the Northwestern Jiaodong Peninsula, China, from SHRIMP U-Pb Zircon Studies of Granitoids.Ore Geology Reviews, 13(1):275-291. https://www.researchgate.net/publication/248211532_Constraints_on_crustal_evolution_and_gold_metallogeny_in_the_Northwestern_Jiaodong_Peninsula_China_from_SHRIMP_U-Pb_zircon_studies_of_granitoids
Wang, Z.L., Yang, L.Q., Guo, L.N., et al., 2015.Fluid Immiscibility and Gold Deposition in the Xincheng Deposit, Jiaodong Peninsula, China:A Fluid Inclusion Study.Ore Geology Reviews, 65:701-717.doi: 10.1016/j.oregeorev.2014.06.006
Wen, B.J., Fan, H.R., Santosh, M., et al., 2015.Genesis of Two Different Types of Gold Mineralization in the Linglong Goldfield, China:Constrains from Geology, Fluid Inclusions and Stable Isotope.Ore Geology Reviews, 65:643-658.doi: 10.1016/j.oregeorev.2014.03.018
Xu, Y.G., 2001.Thermo-Tectonic Destruction of the Archaean Lithospheric Keel beneath the Sino-Korean Craton in China:Evidence, Timing and Mechanism.Physics and Chemistry of the Earth Part A—Solid Earth and Geodesy, 26(9-10):747-757. doi: 10.1016/S1464-1895(01)00124-7
Xu, Y.G., Huang, X.L., Ma, J.L., et al., 2004.Crust-Mantle Interaction during the Tectono-Thermal Reactivation of the North China Craton:Constraints from SHRIMP Zircon U-Pb Chronology and Geochemistry of Mesozoic Plutons from Western Shandong.Contributions to Mineralogy and Petrology, 147(6):750-767. doi: 10.1007/s00410-004-0594-y
Xu, Y.G., Li, H.Y., Pang, C.J., et al., 2009.On the Timing and Duration of the Destruction of the North China Craton.Chinese Science Bulletin, 54(19):3379-3396. https://www.researchgate.net/publication/225642364_On_the_timing_and_duration_of_the_destruction_of_the_North_China_Craton
Zhai, M.G., Meng, Q.R., Liu, J.M., et al., 2004.Geological Features of Mesozoic Tectonic Regime Inversion in Eastern North China and Implication for Geodynamics.Earth Science Frontiers, 11(3):285-297(in Chinese with English abstract). https://www.researchgate.net/publication/312453122_Geological_features_of_Mesozoic_tectonic_regime_inversion_in_Eastern_North_China_and_implication_for_geodynamics
Zhai, Y.S., 2000.Metallogenic System and Its Evolution:From Preliminary Practice to Theoretical Consideration.Earth Science, 25(4):333-339(in Chinese with English abstract). https://trid.trb.org/view.aspx?id=1334916
Zhai, Y.S., Deng, J., Peng, R.M., 2000.Research Contents and Methods for Post-Ore Changes, Modifications and Preservation.Earth Science, 25(4):340-345(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200004001.htm
Zhang, H.F., Li, S.R., Zhai, M.G., et al., 2006.Crust Uplift and Implications in the Jiaodong Peninsula, Eastern China.Acta Petrologica Sinica, 22(2):285-295(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200602003.htm
Zhang, X.O., Cawood, P.A., Wilde, S.A., et al., 2003.Geology and Timing of Mineralization at the Cangshang Gold Deposit, North-Western Jiaodong Peninsula, China.Mineralium Deposita, 38(2):141-153. doi: 10.1007/s00126-002-0290-7
常远, 王玮, 周祖翼, 2010.采样地形对年龄-高程法应用的限制.地球物理学报, 53(8): 1868-1874. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201008013.htm
陈光远, 1993.胶东郭家岭花岗闪长岩成因矿物学与金矿化.武汉:中国地质大学出版社, 131. http://www.cnki.com.cn/Article/CJFDTOTAL-GLGX404.007.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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201012013.htm
陆丽娜, 范宏瑞, 胡芳芳, 等, 2011.胶西北郭家岭花岗闪长岩侵位深度:来自角闪石温压计和流体包裹体的证据.岩石学报, 27(5): 1521-1532. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201105025.htm
吕古贤, 孔庆存, 1993.金矿地质研究丛书:胶东玲珑-焦家式金矿地质.北京:科学出版社, 253. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199100008005.htm
苗来成, 罗镇宽, 黄佳展, 等, 1997.山东招掖金矿带内花岗岩类侵入体锆石SHRIMP研究及其意义.中国科学(D辑), 27(3): 207-213. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199703002.htm
裘有守, 1988.山东招远-掖县地区金矿区域成矿条件.沈阳:辽宁科学技术出版社, 268. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ198400021004.htm
孙华山, 孙林, 曹新志, 等, 2008.胶西北上庄金矿床原生晕轴(垂)向分带特征及深部矿体预测的勘查地球化学标志.矿床地质, 27(1): 64-70. http://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200801008.htm
汪集旸, 黄少鹏, 1990.中国大陆地区大地热流数据汇编(第二版).地震地质, 12(4): 351-366. http://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ199004010.htm
翟明国, 孟庆任, 刘建明, 等, 2004.华北东部中生代构造体制转折峰期的主要地质效应和形成动力学探讨.地学前缘, 11(3): 285-297. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200403036.htm
翟裕生, 2000.成矿系统及其演化——初步实践到理论思考.地球科学, 25(4): 333-339. http://earth-science.net/WebPage/Article.aspx?id=949
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, 25(4): 340-345. http://earth-science.net/WebPage/Article.aspx?id=950
张华锋, 李胜荣, 翟明国, 等, 2006.胶东半岛早白垩世地壳隆升剥蚀及其动力学意义.岩石学报, 22(2): 285-295. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200602003.htm