必须声明标量变量 "@Script_ID"。 四川广元地区朝天剖面上二叠统吴家坪组凝灰岩成因及其地质意义-《地球科学与环境学报》
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[1]张晗,黄虎*,侯明才.四川广元地区朝天剖面上二叠统吴家坪组凝灰岩成因及其地质意义[J].地球科学与环境学报,2020,42(01):36-48.[doi:10.19814/j.jese.2019.08010]
 ZHANG Han,HUANG Hu*,HOU Ming-cai.Origin of Tuffs from Upper Permian Wujiaping Formation in Chaotian Section of Guangyuan Area, Sichuan, China and Its Geological Significance[J].Journal of Earth Sciences and Environment,2020,42(01):36-48.[doi:10.19814/j.jese.2019.08010]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第01期
页码:
36-48
栏目:
基础地质与矿产地质
出版日期:
2020-01-15

文章信息/Info

Title:
Origin of Tuffs from Upper Permian Wujiaping Formation in Chaotian Section of Guangyuan Area, Sichuan, China and Its Geological Significance
文章编号:
1672-6561(2020)01-0036-13
作者:
张晗黄虎*侯明才
(成都理工大学 沉积地质研究院,四川 成都 610059)
Author(s):
ZHANG Han HUANG Hu* HOU Ming-cai
(Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China)
关键词:
地球化学 凝灰岩 锆石U-Pb年龄 Hf同位素 吴家坪组 峨眉山大火成岩省 四川
Keywords:
geochemistry tuff zircon U-Pb age Hf isotope Wujiaping Formation Emeishan large igneous province Sichuan
分类号:
P588.14; P597
DOI:
10.19814/j.jese.2019.08010
文献标志码:
A
摘要:
四川广元地区朝天剖面上二叠统吴家坪组凝灰岩位于茅口组顶部王坡层黏土岩之上,其成因可能对认识峨眉山大火成岩省火山活动时限具有重要意义。对朝天剖面吴家坪组2个凝灰岩样品进行全岩矿物含量、地球化学特征、锆石U-Pb定年、锆石微量元素和Hf同位素分析,探讨凝灰岩的成因,进而讨论其对峨眉山大火成岩省火山活动时限的启示。结果表明:广元地区朝天剖面上二叠统吴家坪组凝灰岩主要由黏土矿物组成,锆石U-Pb年龄为(260.1±2.8)Ma,并具有较高的Al2O3/TiO2值(分别为37.90和31.49)、明显的Eu负异常(Eu/Eu*值分别为0.13和0.06)及缺失Nb、Ta负异常; 凝灰岩样品中,锆石具有较高的εHf(t)值(7.8~11.4)和较低的Th/Nb值(5.4~14.9),与宾川剖面峨眉山火山序列酸性熔结凝灰岩及上寺剖面上二叠统下部凝灰岩基本一致,而明显不同于清音阁王坡层黏土岩锆石εHf(t)值和Th/Nb值。综上所述,四川广元地区朝天剖面上二叠统吴家坪组凝灰岩的形成与峨眉山大火成岩省酸性火山活动有关,且峨眉山大火成岩省的火山活动时限可能一直持续到晚二叠世早期。
Abstract:
The tuffs from Upper Permian Wujiaping Formation in Chaotian section of Guangyuan area, Sichuan are located above Wangpo claystone beds at the top of Maokou Formation, the origin of tuffs may provide a good chance to constrain the age of Emeishan large igneous province volcanism. Mineral contents, whole-rock geochemical characteristics and zircon U-Pb age, trace element and Hf isotopic composition for two tuff samples from Wujiaping Formation in Chaotian section were analyzed to discuss the sources and its geological significance for the age of Emeishan large igneous province volcanism. The results show that the tuffs from Upper Permian Wujiaping Formation in Chaotian section of Guangyuan area with zircon U-Pb age of(260.1±2.8)Ma, are dominated by clay minerals, and have high Al2O3/TiO2 ratios(37.90 and 31.49), strong negative Eu anomalies(Eu/Eu* ratios are 0.13 and 0.06), and no negative Nb and Ta anomalies; zircons from the tuffs have high εHf(t)(7.8-11.4)and low Th/Nb ratios(5.4-14.9); the geochemical characteristics are similar to the lower tuffs from Upper Permian in Shangsi section and the acid ignimbrites of Emeishan volcanic sequence in Binchuan section, but different from the εHf(t)and Th/Nb ratios of Wangpo claystone beds in Qingyinge. In general, the tuffs from Upper Permian Wujiaping Formation in Chaotian section of Guangyuan area, Sichuan are related to the acid volcanism of Emeishan large igneous province, and the age of Emeishan large igneous province volcanism may extend to the early period of Late Permian.

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备注/Memo

备注/Memo:
收稿日期:2019-08-11; 修回日期:2019-11-16; 网络首发日期:2019-12-31投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41502109); 成都理工大学中青年骨干教师计划项目(KYGG201718)
作者简介:张 晗(1994-),男,河南濮阳人,理学硕士研究生,E-mail:z18512858729@163.com。
*通讯作者:黄 虎(1987-),男,湖北宜城人,副教授,博士研究生导师,理学博士,E-mail:118huanghu@163.com。
更新日期/Last Update: 2020-01-07