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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