福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架

潘天望; 袁远; 吕勇; 史文强

doi:10.12090/j.issn.1006-6616.2019.25.01.007

福建紫金山矿田早白垩世以来构造演化和成岩成矿时空格架

doi: 10.12090/j.issn.1006-6616.2019.25.01.007

潘天望^{1, 2,},
袁远^3, ,,
吕勇^{1, 2},
史文强^{1, 2}

1.
中国地质科学院岩溶地质研究所, 广西桂林 541004
2.
自然资源部广西岩溶动力学重点实验室, 广西桂林 541004
3.
中国地质大学(北京) 地球科学与资源学院, 北京 100083

基金项目:

中国地质调查局地质调查项目 DD20160061

中国地质调查局地质调查项目 DD20179313

详细信息

作者简介:
潘天望(1988-), 男, 研究实习员, 主要从事构造地质学与岩溶洞穴景观研究。E-mail:pantianwang@kasrt.ac.cn

通讯作者:
袁远(1989-), 男, 在读博士, 矿田构造专业。E-mail:y_yuan0731@163.com

中图分类号: P548;P612
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- 被引次数: 0
出版历程
- 收稿日期: 2017-10-10
- 修回日期: 2018-05-22
- 刊出日期: 2019-02-28

THE EARLY-CRETACEOUS TECTONIC EVOLUTION AND THE SPATIAL-TEMPORAL FRAMEWORK OF MAGMATISM-MINERALIZATION IN ZIJINSHAN ORE-FIELD, FUJIAN PROVINCE

PAN Tianwang^{1, 2
,},
YUAN Yuan^{3
, ,},
LYU Yong^{1, 2},
SHI Wenqiang^{1, 2}

1.
Institute of Karst Geology, CAGS, Guilin 541004, Guangxi, China
2.
Key Laboratory of Karst Dynamics, MNR & GZAR, Guilin 541004, Guangxi, China
3.
School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China

摘要

摘要: 在充分吸收已有工作成果的基础上，文章系统总结了紫金山矿田的典型矿床类型及特征，探讨了早白垩世伸展构造背景下该矿田成岩成矿作用与北西向上杭—云霄成矿带的关系，并建立了早白垩世（145 Ma~）到晚白垩世早期（~92 Ma）紫金山矿田成岩成矿作用的时空格架。研究认为由于古太平洋板块俯冲作用体系的影响，早白垩世以来（145 Ma~）紫金山矿田总体上受北西向上杭—云霄深断裂多次活化作用的控制，依次经历了145~120 Ma伸展初期小规模的岩浆—成矿活动、125~110 Ma短暂的岩浆间歇期、110~92 Ma幔源物质大规模参与的岩浆活动及相应的斑岩型—浅成低温热液型（Cu-Au-Mo-Ag）多金属成矿作用。
- 构造演化 /
- 成岩成矿关系 /
- 时空分布规律 /
- 紫金山矿田 /
- 上杭-云霄成矿带
Abstract: This paper presents a systematic review of major types and characteristics of the representative deposits in the Zijinshan ore-field by integrating with previous studies, which is in an attempt to establish the spatial-temporal framework of magmatic-metallogenic events during 145~92 Ma time interval and, on that basis, investigate its relationship with the NW-trending Shanghang-Yunxiao mineralization belt under the Early Cretaceous extension setting. We conclude that the magmatism-mineraliztion of the Zijinshan ore-field was mainly controlled by the multiple activation of the NW-trending Shanghang-Yunxiao deep fault in response to Pacific plate subduction. There occurred a small scale of the magmatism and metallogenesis in the Zijinshan ore-field when the regional tectonic regime inversed from compression to extension (145~125 Ma), whereas the intense crust-mantle interaction induced large scale of magmatism and mineralization during the 110~92 Ma in response to the enhanced crust extension, which resulted in generating the giant Zijinshan porphyry-epithermal Cu-Au-Mo-Ag ore system. It's worth noting that a transient tectonic inversion lasted from 125~110 Ma separated the two extension stage mentioned above. These transpression gave rise to the short magmatic quiescence in our study area.
- tectonic evolution /
- the relationship between magmatism and mineralization /
- spatial-temporal framework /
- the Zijinshan ore-field /
- the Shanghang-Yunxiao mineralization belt
注释:

责任编辑：范二平

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图 1 福建上杭—云霄成矿带区域地质与中生代火山盆地分布示意图

a—区域地质简图^[13]；b—中生代火山盆地分布示意图^{[14, 21]}

Figure 1. Tectonic location and regional geological map of Mesozoic Volcanic Basin in the regions of the Shanghang-Yunxiao mineralization belt, Fujian Province

下载: 全尺寸图片幻灯片

图 2 紫金山矿田区域地质简图与地质矿产略图

a—区域地质简图^[15]；b—矿田地质矿产略图^[2]

Figure 2. Regional geological map and mineral map of the Zijinshan ore-field

下载: 全尺寸图片幻灯片

图 3 早白垩世晚期—晚白垩世早期(110~92 Ma)紫金山Cu-Au-Mo-Ag矿田成矿模式图与地球动力学模型简图

a—成矿模式图^[3]; b—地球动力学模型简图^{[6, 34, 67]}

Figure 3. Metallogenic pattern and Cartoon showing the possible tectonic setting for the porphyry-epithermal Cu-Au-Mo-Ag mineralization in the Zijinshan ore-field during 110~92 Ma

下载: 全尺寸图片幻灯片

表 1 上杭紫金山矿田中生代岩浆岩同位素年代一览表

Table 1. Mesozoic magmatic isotope dating of the Zijinshan ore-field

时代	岩体名称	定年方法	测定对象	年龄/Ma	参考文献	相关矿床	定年方法	成因类型	年龄/Ma	参考文献
早—晚白垩世	大岩里花岗斑岩脉	SHRIMP	锆石	93±2	[5]
	紫金山铜金矿床石英斑岩脉	SHRIMP	锆石	96±2	[5]
	浸铜湖石英正长斑岩脉	LA-ICP-MS U-Pb	锆石	95.3±2.1~96.7±0.9	[28]	浸铜湖Cu-Mo矿		斑岩型		[28]
	南山坪正长岩脉	LA-ICP-MS U-Pb	锆石	92.7±1.0	[9]
	南山坪正长斑岩脉	LA-ICP-MS U-Pb	锆石	97.3±1.2	[9]
	南山坪石英正长斑岩脉	LA-ICP-MS U-Pb	锆石	99.5±1.2	[9]
	晚期罗卜岭花岗闪长斑岩	LA-ICP-MS U-Pb	锆石	96.7±2.1	[29]
	罗卜岭深部花岗闪长岩基	SHRIMP	锆石	100±2	[5]	罗卜岭Cu-Mo矿	辉钼矿Re-Os	斑岩型	103~105	[6, 25]
	石帽山群下段气孔状英安岩	SHRIMP	锆石	102±1	[5]
	石帽山群上段上部流纹岩	LA-ICP-MS U-Pb	锆石	102±1	[6]
	紫金山深部花岗闪长岩	SHRIMP	锆石	102±2	[5]
	早期罗卜岭花岗闪长斑岩	LA-ICP-MS U-Pb	锆石	102.9±0.9	[29]
	紫金山深部花岗闪长斑岩	SHRIMP	锆石	103±2	[5]
	早期紫金山铜金矿床英安玢岩	LA-ICP-MS U-Pb	锆石	104±1~104±0.1	[6]
	早期紫金山铜金矿床英安玢岩	LA-ICP-MS U-Pb	锆石	105±0.7	[30]
	石帽山群上段上部流纹质晶屑凝灰岩	LA-ICP-MS U-Pb	锆石	105±0.1	[6]
	石帽山群下段安山岩	SHRIMP	锆石	106±2	[5]
	四方花岗闪长岩	LA-ICP-MS U-Pb	锆石	104.8±1.7	[31]
		Ar-Ar坪年龄	角闪石	104.8±0.8	[11]
		LA-ICP-MS U-Pb	锆石	107±1.8	[11]
		SHRIMP	锆石	109±2	[5]
		LA-ICP-MS U-Pb	锆石	112±1	[6]
	石帽山群下段中部凝灰熔岩	LA-ICP-MS U-Pb	锆石	108±1	[6]
	石帽山群下段上部凝灰岩	LA-ICP-MS U-Pb	锆石	110±1	[6]
	石帽山群上组下段流纹岩	LA-ICP-MS U-Pb	锆石	110.0±1.9	[4]
	紫金山铜金矿床英安玢岩	LA-ICP-MS U-Pb	锆石	110±0.4	[6]
	紫金山次火山岩	锆石U-Pb	锆石	118±4	[32]	有待考证
	石帽山群下组下段英安岩	LA-ICP-MS U-Pb	锆石	111±0.3~110±1	[6]
	石帽山群下段底部熔结角砾(集块)岩	LA-ICP-MS U-Pb	锆石	113.0±1.9	[4]
中—晚侏罗世	才溪中粗粒似斑状二长花岗岩	LA-ICP-MS U-Pb	锆石	146.4±8.6	[31]
		SHRIMP	锆石	150±2	[5]
		SHRIMP	锆石	150±3	[30]
	金龙桥细粒花岗岩	LA-ICP-MS U-Pb	锆石	157±1	[6]
		LA-ICP-MS U-Pb	锆石	155	[33]
		SHRIMP	锆石	149±2	[5]
		LA-ICP-MS U-Pb	锆石	146.3±1.6	[4]
	五龙寺中细粒花岗岩	LA-ICP-MS U-Pb	锆石	164±1	[6]
		LA-ICP-MS U-Pb	锆石	163	[33]
		LA-ICP-MS U-Pb	锆石	149.3±1.6	[4]
		SHRIMP	锆石	149±2	[5]
	迳美中粗粒花岗岩	LA-ICP-MS U-Pb	锆石	165±1	[6]
		LA-ICP-MS U-Pb	锆石	164	[33]
		LA-ICP-MS U-Pb	锆石	157.9±1.2	[4]
		SHRIMP	锆石	154±2	[5]
	溪南二长花岗岩	LA-ICP-MS U-Pb	锆石	156.9±1.0	[34]	溪南Cu-Mo矿	辉钼矿Re-Os	斑岩型	108	[34]

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表 2 紫金山矿田燕山期构造演化一览表

Table 2. Yanshanian tectonic evolution of the Zijinshan ore-field

构造演化阶段	地质时代	代表性岩体(脉)	岩石成因	构造背景
燕山晚期	早白垩世早期(145~120 Ma)	外围大洋-莒舟岩体	壳源岩石重熔，少量幔源组分参与	伸展构造背景(转换过渡)
	早白垩世中期(120~110 Ma)	岩浆间歇期	——	短暂的构造反转
	早白垩世晚期(110~92 Ma)	四方岩体；罗卜岭岩体；大岩里花岗斑岩脉；紫金山石英斑岩脉；浸铜湖石英正长斑岩脉	地幔组分逐渐增多，具典型的壳幔混源型花岗岩特征	伸展环境，伸展作用逐渐加强，期间可能经历了短暂构造反转，

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