地震地质

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琼北峨蔓地区第四纪火山活动研究

杨文健1,赵波1,于红梅1,许建东1,潘波1,王锡娇2   

  1. 1. 中国地震局地质研究所
    2. 中国地质大学(北京)
  • 收稿日期:2021-05-08 修回日期:2021-06-16 发布日期:2021-09-26
  • 通讯作者: 赵波
  • 基金资助:
    中国地震局地质研究所基本科研业务专项

STUDY ON QUATERNARY VOLCANISM IN EMAN AREA, NORTHERN HAINAN ISLAND

  • Received:2021-05-08 Revised:2021-06-16 Published:2021-09-26
  • Contact: Bo Zhao

摘要: 琼北作为我国最大的第四纪火山区之一,其火山活动表现出多期、多旋回特征,但位于其西北角的峨蔓火山岩的喷发时代依然存在争议。本文对峨蔓火山区展开了详细的火山地质及地貌调查,并结合全岩主量元素分析,以及火山岩K-Ar年代学和贝壳14C年代学研究,以揭示其火山活动时代和喷发特征等。峨蔓火山区具有笔架岭、春历岭、兵马角、龙门激浪、龙门灯塔以及张屋村等火山,其火山喷发方式主要为溢流式喷发、射汽-岩浆爆破式喷发和弱岩浆爆破式喷发。熔岩流几乎遍及整个火山区,分布面积约26.3km2;基浪堆积物、溅落堆积物以及火山渣分布较小,仅限于龙门激浪-五彩湾和张屋村附近。峨蔓火山岩成分变化较大,整体偏中性,主要由玄武安山岩、玄武岩粗安岩和粗安岩组成,在岩浆演化过程经历了橄榄石和单斜辉石的结晶分异。综合火山岩风化程度(球形风化、红土层)、火山地质与地貌特征(锥体形貌、坡度)、岩石学和地球化学特征(橄榄石斑晶蚀变、全岩成分差异)以及K-Ar年龄(0.12~0.44 Ma)和贝壳14C年龄(43.27±0.67 ka BP)结果显示,峨蔓火山区的火山活动时代应属于中、晚更新世。

关键词: 第四纪火山, 喷发方式 , 喷发时代 , 琼北火山群 , 峨蔓

Abstract: As one of the largest Quaternary volcanic clusters in China, the volcanic activities of Qiongbei are characterized by multi-stage and multi-cycle, however, the eruption era of Eman volcanic rock located in the northwest of Qiongbei volcanic cluster is still controversial. Here, we present a comprehensive study of volcanic geology and geomorphology, whole-rock major elements, K-Ar geochronology of volcanic rocks and 14C geochronology of conch, in order to revel the epoch of volcanic activity and eruption characteristics of Eman volcanic field. There are many craters, such as Bijialing, Chunliling, Bingmajiao, Longmenjilang, Longmen pharos, and Zhangwu. The main types of volcanic eruption are effusive eruptions, phreatomagmatic explosive eruptions and weakly magmatic explosive eruptions. Lava flows almost cover the entire volcanic field, with an area of about 26.3km2. However, base-surge deposits, spattering deposits and scoria are only distributed in the vicinity of Longmenjilang-Wucaiwan and Zhangwu Village. The composition of Eman volcanic rocks varies greatly and is generally intermediate, which is mainly composed of basaltic andesite, basaltic trachyandesite and trachyandesite, and experiences fractional crystallization of olivine and clinopyroxene in the process of magmatic evolution. we based on the weathering degree of volcanic rocks (spherical weathering, red clay layer), volcanic geology and geomorphology (cone morphology, slope), petrology and petrogeochemistry (difference of major elements, olivine phenocryst alteration), K-Ar age of volcanic rocks (0.12~0.44 Ma) and 14C age of conch (43.27±0.67 ka.BP), it is concluded that the eruption era in Eman volcanic field belongs to the Middle and Late Pleistocene.

Key words: Quaternary volcano, eruption type, eruption era, Qiongbei volcanic clusters, Eman