地学前缘 ›› 2021, Vol. 28 ›› Issue (1): 353-362.DOI: 10.13745/j.esf.sf.2020.11.29

• 非主题来稿选登 • 上一篇    下一篇

河北武安地区隐爆角砾岩特征及成因探讨

李瑞鹏1,2(), 崔晓亮1, 苏尚国1,*(), 张雅南1, 梁存涛1, 陈学根1   

  1. 1. 中国地质大学(北京) 地球科学与资源学院, 北京 100083
    2. 深圳云创瑞诚数据科技有限公司, 广东 深圳 518101
  • 收稿日期:2020-01-10 修回日期:2020-12-04 出版日期:2021-01-25 发布日期:2021-01-28
  • 通讯作者: 苏尚国
  • 作者简介:李瑞鹏(1984—),男,硕士,高级工程师,矿物学、岩石学、矿床学专业。E-mail: liruipengcugb@126.com
  • 基金资助:
    国家自然科学基金项目(41272105);中国地质调查局地质调查项目(12120115069701)

Discussion on the features and mechanism of cryptoexplosive breccia in Wu’an, Hebei Province

LI Ruipeng1,2(), CUI Xiaoliang1, SU Shangguo1,*(), ZHANG Yanan1, LIANG Cuntao1, CHEN Xuegen1   

  1. 1. School of Earth Sciences and Resources,China University of Geosciences(Beijing), Beijing 100083, China
    2. YunchuangRuiCheng Data Technology Ltd. Company, Shenzhen 518101, China
  • Received:2020-01-10 Revised:2020-12-04 Online:2021-01-25 Published:2021-01-28
  • Contact: SU Shangguo

摘要:

出露于河北武安地区的隐爆角砾岩分布广泛,其成岩过程对于研究该区岩浆和流体的相互作用及成矿作用具有重要意义。本文对河北武安洪山隐爆角砾岩进行了详细的野外及镜下观察及电子探针(EMPA)及激光剥蚀等离子质谱仪(LA-ICP-MS)的原位分析。详细的矿物学研究表明,武安角砾岩主要分布于主岩体(闪长岩)与围岩(灰岩)之间,角砾多为棱角状、次棱角状,具有明显可以拼合的特征,角砾边部常可见方解石的再生加大现象,因铁含量的不同,角砾呈深浅不同的颜色。基质成分主要由方解石和赤铁矿组成。赤铁矿环带发育,其核部FeO高,边部MgO、Al2O3高,其全铁含量与SiO2呈良好的负相关关系;赤铁矿相对富集Ba,K,U等元素,亏损Th,Ta,Nb,Zr,Hf等高场强元素,表明其可能形成于岩浆-流体环境。同心层状赤铁矿明显富集Ti和Pb,Ti的相对富集表明同心层状赤铁矿的成因与岩浆有关,Pb的相对富集则表明其形成后期有热液叠加参与。本文研究认为,武安地区隐爆角砾岩的成因模式为:深部岩浆流体在上升过程中受到上覆围岩的圈闭而产生流体沸腾超压现象,随后上覆岩层突然减压破碎,岩浆-流体发生隐爆作用并将上层岩体破碎胶结成岩。

关键词: 河北武安, 隐爆角砾岩, 岩浆热液, 赤铁矿

Abstract:

Cryptoexplosive breccia is widely distributed in Wu’an, Hebei Province. The study of its forming process of is important to the understandings of the interaction between magma and fluid and the formation of Fe deposit. We carried out in situ mineralogical analysis by electron microprobe analysis (EMPA) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) in combination with detailed field and microscope investigation. The results show that the Wu’an breccia is mainly distributed between the Hongshan intrusive complex (mainly diorite) and its host rock (limestone). The gravels are mostly angular or subangular-shaped and could be easily pieced together. Secondary enlargement of calcite is often seen on the edge of the angular gravels of different colors due to different Fe contents. The matrix of breccia is mainly composed of calcite and hematite. A composition zone can be observed in hematite, which has higher FeO content in the core and higher MgO and Al2O3 contents in the edge. The total iron is negatively correlated with SiO2 content. The trace elemental characteristics of hematite show enrichments of Ba, K and U and depletions of high field-strength elements, such as Th, Ta, Nb, Zr and Hf, which may indicate that the magma was formed in a magma-fluid environment. The core hematite zone is enriched in Ti and Pb. The enrichment of Ti indicates the hematite’s magmatic origin, while the enrichment of Pb indicates a later involvement of hydrofluid superposition. According to this study, the genetic model of the cryptoexplosive breccia in the Wu’an area is as follows: The trapping of rising deep magmatic fluid by overlying host rock resulted in boiling and overpressure of the fluid, which led to cryptoexplosion as the overlying rock strata suddenly decompressed and broke up and the magmatic fluid cemented the upper rock mass into rocks.

Key words: Wu’an City in Hebei Province;, cryptoexplosive breccia, magmatic hydrothermal fluid, hematite

中图分类号: