雷州半岛中西部第四纪火山岩的<sup>40</sup>Ar/<sup>39</sup>Ar年龄及地质意义

李响; 张宗言; 李海勇; 张楗钰; 白秀娟

doi:10.12090/j.issn.1006-6616.2023098

雷州半岛中西部第四纪火山岩的⁴⁰Ar/³⁹Ar年龄及地质意义

doi: 10.12090/j.issn.1006-6616.2023098

李响^{1, 2,},
张宗言^{1, 2},
李海勇^{3, 4, ,},
张楗钰¹,
白秀娟⁵

1.
中国地质调查局武汉地质调查中心，湖北武汉 430205
2.
中国地质调查局花岗岩成岩成矿研究中心，湖北武汉 430205
3.
中国科学院南海海洋研究所，广东广州 511458
4.
中国科学院边缘海与大洋地质重点实验室，广东广州 511458
5.
中国地质大学（武汉）资源学院，构造与油气资源教育部重点实验室，湖北武汉 430074

基金项目: 中国地质调查局地质调查项目（DD20230204，DD20221634，DD20160035）；珠海市城市地质调查（含信息化）项目（MZCD-2201-008）；广东省基础与应用基础研究基金（2019A1515011244）；广州市基础与应用基础研究基金（202201010720）；国家自然科学基金项目（91958212）

详细信息

作者简介:
李响（1983—），男，博士，正高级工程师，主要从事成因矿物学和第四纪地质研究。E-mail：lixiang_503@163.com

通讯作者:
李海勇（1982—），男，博士，副研究员，主要从事研究方向为海洋地球化学研究。E-mail：hyli@scsio.ac.cn

中图分类号: P597；P534
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出版历程
- 收稿日期: 2023-06-14
- 修回日期: 2023-07-05
- 录用日期: 2023-07-17

⁴⁰Ar/³⁹Ar ages of Quaternary volcanic rocks from the midwest of the Leizhou Peninsula, and their geologic significance

LI Xiang^{1, 2
,},
ZHANG Zongyan^{1, 2},
LI Haiyong^{3, 4
, ,},
ZHANG Jianyu¹,
BAI Xiujuan⁵

1.
Wuhan Center of China Geological Survey, Wuhan 430205, Hubei, China
2.
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China
3.
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 511458, Guangdong, China
4.
Key Laboratory of Ocean and Marginal Sea Geology, Guangzhou 511458, Guangdong, China
5.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

Funds: This research is financially supported by the Geological Survey Project of the China Geological Survey (Grants DD20230204, DD20221634, and DD20160035), the Zhuhai Urban Geological Survey (including information) Project (Grant MZCD-2201-008), the Guangdong Basic and Applied Basic Research Foundation (Grant 2019A1515011244), the Guangzhou Basic and Applied Basic Research Fund (Grant 202201010720), and the National Natural Science Foundation of China (Grant No. 91958212).

摘要

摘要:
雷州半岛地区第四纪火山岩广泛分布，但对火山岩形成的时代还存在争议。文章利用高精度的激光阶段加热⁴⁰Ar/³⁹Ar法对雷州半岛中西部火山岩的年龄进行了测定，并结合与相邻地层的接触关系，划分了2个火山活动旋回。第Ⅰ旋回火山岩呈夹层产于湛江组内部，仅见于钻孔ZKC12中，岩性为橄榄拉斑玄武岩；第Ⅱ旋回火山岩在区内分布最广，覆盖在湛江组之上，⁴⁰Ar/³⁹Ar年龄为2.02～0.88 Ma，时代为早更新世早期至早更新世晚期，结合与周围地层的接触关系，进一步划分为4个喷发期。第1喷发期（Ⅱ₁）规模最大，出露面积最广，形成2个喷发中心，⁴⁰Ar/³⁹Ar年龄为2.02±0.03 Ma；第2喷发期（Ⅱ₂）主要分布于锅盖岭和北插一带，⁴⁰Ar/³⁹Ar年龄分别为1.77±0.03 Ma、1.70±0.03 Ma；第3喷发期（Ⅱ₃）喷发中心位于火炬农场，⁴⁰Ar/³⁹Ar年龄为1.51±0.07 Ma；第4喷发期（Ⅱ₄）岩性以沿裂隙喷发形成的溢流相的玄武质熔岩为主， ⁴⁰Ar/³⁹Ar年龄为0.88±0.14 Ma。火山活动明显受北东向和北西向基底断裂的控制。研究成果为雷州半岛地区火山活动时代、期次和活动规律研究提供了重要年龄证据。
- 火山岩 /
- ⁴⁰Ar/³⁹Ar 法 /
- 火山旋回 /
- 第四纪 /
- 雷州半岛 /
- 年代学
Abstract:
Quaternary volcanic rocks are widely distributed in the Leizhou Peninsula, but the age of volcanic formation remains controversial. This study used the high-precision laser stepwise heating 40Ar/39Ar method to date the age of volcanic samples from the midwest of the Leizhou Peninsula, and two volcanic cycles were determined by combining the contact relationship with the neighboring strata. Volcanic rocks of the first cycle (Ⅰ) occur as interlayers in the Zhanjiang Formation, only seen in Borehole ZKC12, and the lithology is olivine tholeiite; volcanic rocks of the second cycle (Ⅱ) are the most widely distributed in the study area, unconformably overlaying on the Zhanjiang Formation, with ⁴⁰Ar/³⁹Ar ages ranging from 2.02 to 0.88 Ma, indicating that they were erupted from the early stage of the early Pleistocene to the end of the early Pleistocene. On the combination of contact relationship with surrounding strata, the second cycle can be further divided into four eruption stages. The first eruption stage (Ⅱ₁) has the largest scale and the most extensive area, forming two eruption centers with ⁴⁰Ar/³⁹Ar age of 2.02±0.03 Ma. The second eruption stage (Ⅱ₂) centers in the areas of Guokailing and Beicha with 40Ar/39Ar ages of 1.77±0.03 Ma and 1.70±0.03 Ma, respectively. The eruptional center of the third eruption stage (Ⅱ₃) lies at Huoju Farm, and the age of ⁴⁰Ar/³⁹Ar is 1.51±0.07 Ma. The lithology of the fourth eruption stage (Ⅱ₄) is dominated by basaltic lava of overflow phase formed by fissure eruption, and the ⁴⁰Ar/³⁹Ar age is 0.88±0.14 Ma. The volcanic activity is obviously controlled by NE-trending and NW-trending basement faults. These results provide reliable age data to constrain Leizhou Peninsula’s forming age, eruption periods, and the law of volcanic activity.
- volcanic rocks /
- ⁴⁰Ar/³⁹Ar method /
- volcanic cycles /
- Quaternary /
- Leizhou Peninsula /
- geochronology

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图 1 雷州半岛中西部火山岩分期分布图

a—雷州半岛第四纪地质简图；b—研究区火山岩分期分布图

Figure 1. Distribution of volcanic rocks in the midwest of the Leizhou Peninsula

(a) Quaternary geological sketch map of the Leizhou Peninsula; (b) Staged distribution of volcanic rocks in the study area

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图 2 代表性钻孔及⁴⁰Ar/³⁹Ar年龄样采样层位

Figure 2. Representative drill cores and ⁴⁰Ar/³⁹Ar age sampling horizons in the study area

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图 3 雷州半岛中西部火山岩⁴⁰Ar/³⁹Ar年龄谱和反等时线

Figure 3. Age spectra (left) and inverse isochrons (right) of volcanic rock samples from the midwest of the Leizhou Peninsula by ⁴⁰Ar/³⁹Ar laser stepwise heating

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图 4 雷州半岛中西部火山岩野外地质特征

a—石峁岭组火山岩呈喷发不整合覆盖在湛江组之上；b—草罗岭采石场火山岩中的喷发韵律，红土夹层代表喷发间断；c—玄武岩球形风化；d—玄武岩中的绳状构造

Figure 4. Field geological characteristics of volcanic rocks in the midwest of the Leizhou Peninsula

(a) Volcanic rocks of the Shimaoling formation unconformably overlying the the Zhanjiang formation; (b) eruptive rhythmites in the volcanic rocks of Caoluoling Quarry, with red clay interlayers representing eruptive discontinuities; (c) Spherical weathering of basalt; (d) Ropy structure in basalt

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表 1 雷州半岛中西部火山活动旋回划分表

Table 1. Division of volcanic eruption cycles in the midwest of the Leizhou Peninsula

地质年代		旋回	喷发期	产出层位	累计厚度/m	出露面积/km²	主要岩性	火山岩相	同位素年龄/Ma
纪	世	旋回	喷发期	产出层位	累计厚度/m	出露面积/km²	主要岩性	火山岩相	同位素年龄/Ma
第四纪	更新世	Ⅱ	Ⅱ₄	石峁岭组	>4 .0m	4.1	橄榄拉斑玄武岩	溢流相	0.88
			Ⅱ₃		>200.0 m	10.8	石英拉斑玄武岩	溢流相	1.51
			Ⅱ₂		>101.4 m	34.3	石英拉斑玄武岩、火山碎屑岩	溢流相爆发相	1.70～1.77
			Ⅱ₁		>33.5 m	126.1	石英拉斑玄武岩、火山碎屑岩	溢流相爆发相	2.02
		Ⅰ		湛江组	>7.4 m	无出露	橄榄拉斑玄武岩	溢流相

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