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长白山天池火山造锥阶段玄武质火山活动期次划分及成因探讨

钱程, 崔天日, 唐振, 江斌, 张超, 秦涛, 陆露, 陈会军, 吴桐

钱程, 崔天日, 唐振, 江斌, 张超, 秦涛, 陆露, 陈会军, 吴桐. 长白山天池火山造锥阶段玄武质火山活动期次划分及成因探讨[J]. 中国地质, 2016, 43(6): 1963-1976. DOI: 10.12029/gc20160608
引用本文: 钱程, 崔天日, 唐振, 江斌, 张超, 秦涛, 陆露, 陈会军, 吴桐. 长白山天池火山造锥阶段玄武质火山活动期次划分及成因探讨[J]. 中国地质, 2016, 43(6): 1963-1976. DOI: 10.12029/gc20160608
QIAN Cheng, CUI Tian-ri, TANG Zhen, JIANG Bin, ZHANG Chao, QIN Tao, LU Lu, CHEN Hui-jun, WU Tong. Stage division and genesis discussion of basaltic volcanism during the coneforming stage of Tianchi volcano in Changbaishan region[J]. GEOLOGY IN CHINA, 2016, 43(6): 1963-1976. DOI: 10.12029/gc20160608
Citation: QIAN Cheng, CUI Tian-ri, TANG Zhen, JIANG Bin, ZHANG Chao, QIN Tao, LU Lu, CHEN Hui-jun, WU Tong. Stage division and genesis discussion of basaltic volcanism during the coneforming stage of Tianchi volcano in Changbaishan region[J]. GEOLOGY IN CHINA, 2016, 43(6): 1963-1976. DOI: 10.12029/gc20160608

长白山天池火山造锥阶段玄武质火山活动期次划分及成因探讨

基金项目: 

国土资源部公益性行业基金项目“长白山火山基础地质与环境地质研究” 201211095-5

中国地质调查局项目“东北重大岩浆事件及其成矿作用与构造背景综合研究” 12120114085601

详细信息
    作者简介:

    钱程, 男, 1985年生, 硕士, 工程师, 构造地质学专业, 主要从事区域地质与中新生代构造研究; E-mail:qch1985123@163.com

  • 中图分类号: P588.14

Stage division and genesis discussion of basaltic volcanism during the coneforming stage of Tianchi volcano in Changbaishan region

Funds: 

Ministry of Land and Resources Public Welfare Industry Fund Program 201211095-5

China Geological Survey Program 12120114085601

More Information
    Author Bio:

    QIAN Cheng, male, born in 1985, engineer, master, engages in the study of regional geology and Mesozoic-Neozoic tectonics; E-mail:qch1985123@163.com

  • 摘要:

    在天池火山造锥阶段,长白山火山区玄武质火山活动频繁。文章在野外调查的基础上,通过年代学及地球化学研究,对其活动期次进行划分,并探讨其岩浆来源与演化。天池火山造锥阶段的玄武质火山岩主要呈火山渣锥或小型河谷玄武岩形式分布,其形成可划分为两期:一期为老房子小山期,形成时限为0.87~0.54 Ma,属碱性岩石系列;另一期为老虎洞期,形成时限为0.34~0.1 Ma,属碱性岩石系列和拉斑岩石系列。地球化学特征显示,碱性系列玄武岩具高Al、Ti、K、P和低Mg特征,拉斑系列玄武岩具高Mg、富Fe、Ca和低Na特征;二者稀土和微量特征较为一致,稀土元素配分曲线呈右倾型,略显正铕异常,并富集Ba、K、Pb、P、Ti,亏损Th、U、Sr,但拉斑系列玄武岩的稀土元素和微量元素含量及轻重稀土分馏强度均低于碱性系列。天池火山造锥阶段形成的玄武质火山岩均来源于进化岩浆,具有同源特征,经历了一致或相似的演化过程,岩浆房赋存位置相当于上地幔-下地壳的过渡部位,结晶分异岩浆作用显著、地壳混染作用微弱,其成分变化受控于多期次结晶分异作用和早期结晶再循环的岩浆作用过程。

    Abstract:

    During the cone-forming stage of Tianchi volcano, activity of basaltic volcanism was frequent. In this paper, based on field geological survey and analysis of chronology and geochemistry, the authors determined active stages of the basaltic volcanism, and investigated magmatic source and evolution. The results show that the activity of the basaltic volcanism forming scoria cones or mini valley basalt can be divided into 2 stages:Laofangzixiaoshan period (about 0.87-0.54 Ma) belonging to alkaline basaltic volcanism and Laohudong period (about 0.34-0.1 Ma) belonging to alkaline and tholeiitic volcanism. Alkaline basalt is rich in Al, Ti, K and P, and poor in Mg, and tholeiite is rich in Mg, Fe and Ca, and poor in Na. The two types of basalt have similar characteristics in REEs, trace elements and Eu anomalies, exhibiting obvious right-declined REE patterns, slightly positive Eu anomalies, enrichment of Ba, K, Pb, P and Ti, and depletion in Th, U and Sr. Nevertheless, in contrast to alkaline basalt, content of REEs and trace elements, and fractional degree of HREE and LREE are lower in tholeiite. The basalt formed during the coneforming stage of Tianchi volcano was derived from evolutional magma, and was identical with the transitional position of uppermantle and lower-crust, which had characteristics of common fountain, and had the same or similar evolution process with significant crystallization differentiation and faint crustal contamination. Compositions of the evolutional magma were controlled by multi-stages crystallization differentiation and recirculation during early crystallization.

  • 图  1   研究区地质简图(据[21]修改)

    1-全新世火山喷发物;2-早更新世晚期-晚更新世粗面岩;3-中更新世粗面岩;4-早更新世粗面岩;5-早更新世晚期-晚更新世玄武岩;6-上新世-早更新世早期玄武岩;7-中新世玄武岩;8-破火山口;9-本次采样点位置及编号;10-前人采样点及K-Ar测年结果

    Figure  1.   Geological map of the study area (modified after reference [21])

    1-Holocene eruptive material; 2-Late stage of Early Pleistocene -Late Pleistocene trachyte, 3-Maddle Pleistocene trachyte; 4-Early Pleistocene trachyte; 5-Late stage of Early Pleistocene -Late Pleistocene basalt; 6-Pliocene -early stage of Early Pleistocene basalt; 7-Miocene basalt; 8-Caldera; 9-Sampling position and serial number; 10-Previous sampling positions and their K-Ar dating results

    图  2   野外岩貌和显微薄片照片

    a-C1535采样点露头及采样位置;b-C528采样点露头及采样位置;c-C1535-2显微薄片特征,单偏光;d-C528-1显微薄片特征,正交偏光;Ol-橄榄石;Cpx-单斜辉石;P-斜长石

    Figure  2.   Photos of rock morphology and micro-section

    a-C1535 sampling point outcrop and sampling position; b-C528 sampling point outcrop and sampling position; c-C1535-2 micro-section (plainlight); d-C528-1 micro-section (crossed nicols) Ol-Olivine; Cpx-Clinopyroxene; Pl-Plagioclase

    图  3   CZK05岩心柱状图和显微薄片照片

    a-CZK05钻岩芯及采样位置;b-CZK05-1显微薄片特征,单偏光;Pl-斜长石

    Figure  3.   CZK05 drilling core columnar and micro-section photo

    a-CZK05 drilling core columnar and sampling position; b-CZK05-1 micro-section (plainlight); Pl-Plagioclase

    图  4   SiO2-Na2O+K2O图和SiO2-FeT/MgO图(前人数据来源见表 3

    Figure  4.   Plots of SiO2 versus Na2O+K2O and SiO2 versus FeT/MgO (data after Table 3)

    图  5   稀土元素标准化曲线和微量元素蛛网图(前人数据来源见表 3)(标准化值据[26])

    Figure  5.   Chondrite-normalized REE patterns and primitive mantle-normalized trace element spider diagrams (data after Table 3) (normalization values after reference [26])

    图  6   La-Ce、La-Nb、La-La/Sm、Ce-Ce/Yb、Ta-Tb及Yb/Y-Rb/Y相关图(前人数据来源见表 3),(c、d虚线来源于[9])

    Figure  6.   Plots of La versus Ce, La versus Nb, La versus La/Sm, Ce versus Ce/Yb, Ta versus Tb and Yb/Y versus Rb/Y (data after Table 3; Trend lines in c and d after [9])

    图  7   MgO与其他主量元素、部分微量元素及特征参数的相关图(前人数据来源见表 3

    实线箭头代表老虎洞期岩浆演化趋势;虚线箭头表示老房子小山期岩浆演化趋势

    Figure  7.   Plots of major elements, some trace elements and characteristic parameters against MgO (data after Table 3)

    Real lines are evolution trends of magma at Laohudong stage, dashed lines are evolution trends of magma at Laofangzixiaoshan stage

    表  1   本次K-Ar测年结果

    Table  1   The K-Ar ages of basalt

    下载: 导出CSV

    表  2   长白山天池火山造锥阶段玄武质火山岩K-Ar测年结果

    Table  2   The K-Ar ages of basaltic rocks formed during the cone-forming stage of Tianchi volcano

    下载: 导出CSV

    表  3   长白山天池火山造锥阶段玄武质火山岩岩石地球化学数据及特征参数

    Table  3   Geochemical data and characteristic parameters of basaltic rocks formed during the cone-forming stage of Tianchi volcano

    下载: 导出CSV
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出版历程
  • 收稿日期:  2015-12-03
  • 修回日期:  2016-03-10
  • 网络出版日期:  2023-09-25
  • 刊出日期:  2016-12-24

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