[1]褚平利,靳国栋,张炜,等.浙江苍南望州山破火山地质特征及其形成演化[J].华东地质,2022,43(04):460-473.[doi:10.16788/j.hddz.32-1865/P.2022.04.006]
 CHU Pingli,JIN Guodong,ZHANG Wei,et al.Geologic features and evolution of Wangzhoushan caldera in Cangnan County, Zhejiang Province[J].East China Geology,2022,43(04):460-473.[doi:10.16788/j.hddz.32-1865/P.2022.04.006]
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浙江苍南望州山破火山地质特征及其形成演化()
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《华东地质》[ISSN:2096-1871/CN:32-1865/P]

卷:
43
期数:
2022年04期
页码:
460-473
栏目:
火山岩填图技术与古火山解剖
出版日期:
2022-12-23

文章信息/Info

Title:
Geologic features and evolution of Wangzhoushan caldera in Cangnan County, Zhejiang Province
作者:
褚平利123 靳国栋2 张炜2 陈荣2 范飞鹏2 段政12 余明刚2 赵希林23 李龙明3 贺振宇4
1. 中国地质科学院地质研究所, 北京 100037;
2. 中国地质调查局南京地质调查中心, 江苏 南京 210016;
3. 合肥工业大学资源与环境工程学院, 安徽 合肥 230009;
4. 北京科技大学土木与资源工程学院, 北京 100083
Author(s):
CHU Pingli123 JIN Guodong2 ZHANG Wei2 CHEN Rong2 FAN Feipeng2 DUAN Zheng12 YU Minggang2 ZHAO Xilin23 LI Longming3 HE Zhenyu4
1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2. Nanjing Center, China Geological Survey, Nanjing 210016, Jiangsu, China;
3. Department of Resources and Environment Hefei University of Technology, Hefei 230009, Anhui, China;
4. School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
关键词:
望州山复活破火山火山演化火山岩相火山断裂构造浙江苍南
Keywords:
Wangzhoushan resurgent calderavolcanic evolutionvolcanic lithofaciesvolcanic faultsCangnan County in Zhejiang Province
分类号:
P588.14P52
DOI:
10.16788/j.hddz.32-1865/P.2022.04.006
摘要:
相对于保存完好的新火山而言,古老火山由于经受长期剥蚀与后期构造改造能够直接出露不同时期和深度的物质组成,是火山机构解剖的理想对象。通过对古火山机构进行调查及研究,对于理解火山喷发过程和浅部岩浆系统演化具有重要研究意义,同时对活动火山的监测及灾害评估具有实践意义。文章通过系统的野外地质调查和综合研究,对浙江苍南地区望州山古火山进行了详细的剖析,根据岩性岩相平面上呈环状展布且向核部由老变新,产状围斜内倾,发育典型的环状、放射状断层以及晚期中央侵入相岩穹等特征,确认其是一座典型的复活破火山,其形成演化先后经历了初始断陷与小规模喷发、普林尼式喷发、溢流式喷发、大规模普林尼式喷发和破火山塌陷、晚期复活5个阶段。
Abstract:
Compared with the well-preserved young volcanoes, the ancient volcanoes that have experienced long denudation and late structural transformation can directly expose the material composition of different forming time and depth, which is the ideal object for the anatomy of volcanic edifice. It plays an important role for understanding the process of volcanic eruption and the evolution of shallow magma system, and has practical significance for the monitoring and disaster assessment of active volcanoes. Based on regional geological survey and comprehensive research of Wangzhoushan ancient volcano in Cangnan, Zhejiang Province, we identify that this ancient volcano is a typical resurgent caldera according to its lithology and lithofacies plane which show annular distribution and become younger toward the core with the occurrence of inward-dipping volcano-sedimentary strata, typical ring and radial faults, and later resurgent dome. The evolution of Wangzhoushan caldera consists of six stages: initial subsidence accompanied with small eruptions, minor Plinian eruption, effusive eruption, major Plinian eruption, caldera collapse and resurgence.

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备注/Memo

备注/Memo:
收稿日期:2022-05-25;改回日期:2022-09-11。
基金项目:中国地质调查局"武夷山松溪-庆元地区区域地质调查(编号:DD20190045)"、"华东地区区域基础地质调查(编号:DD20221633)"和国家自然科学基金"酸性火山岩的成分分层与地壳岩浆系统演化(编号:42172070)"项目联合资助。
作者简介:褚平利,1985年生,男,高级工程师,博士研究生,主要从事火山岩地质调查与研究工作。Email:343938990@qq.com。
通讯作者:贺振宇,1976年生,男,教授,博士,博士生导师,主要从事火成岩岩石学研究工作。Email:zhenyuhe@ustb.edu.cn。
更新日期/Last Update: 1900-01-01