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现代矿业 ›› 2022, Vol. 38 ›› Issue (07): 20-.

• 地质·测量 • 上一篇    下一篇

黑龙江省北部新元古代—早石炭世洋—陆转换过程

张铁安 赵雨生 高洪岩 刘宇奇 刘宇崴 杜兵盈   

  1. 黑龙江省地质科学研究所
  • 出版日期:2022-07-25 发布日期:2023-06-07
  • 基金资助:
    *中国地质调查局地质调查子课题(编号:12120114033501)。

Neoproterozoic-early Carboniferous Ocean-land Transformation in the North of Heilongjiang Province

ZHANG Tie'an ZHAO Yusheng GAO Hongyan LIU Yuqi LIU Yuwei DU Bingying   

  1. Heilongjiang Geological Science Institute
  • Online:2022-07-25 Published:2023-06-07

摘要: 针对东北微地块群拼贴位置及构造演化这一重要科学问题,运用洋—陆转换及大陆 动力学等地学理论,通过系统分析额尔古纳—松嫩地块间新元古代—早寒武世新林—塔源—兴隆 俯冲增生杂岩带、早石炭世嫩江—黑河俯冲增生杂岩带的物质组成,甄别出了俯冲增生杂岩带内 蛇绿岩的类型及构造环境。研究表明:新元古代—早寒武世新林—塔源—兴隆俯冲增生杂岩蛇绿 岩类型主要包括SSZ 型蛇绿岩—富铌基性火山岩,地幔柱型蛇绿岩—超镁铁质岩、辉长岩组合,与 弧—盆演化相关的蛇绿岩超镁铁质岩、辉长岩组合;早石炭世嫩江—黑河俯冲增生杂岩蛇绿岩类 型主要是与弧—盆演化相关的超镁铁质岩、辉长岩组合。结合新元古代—早寒武世新林—塔源— 兴隆俯冲增生杂岩带、早石炭世嫩江—黑河俯冲增生杂岩带的物质组成和各期岩浆弧、区域磨拉 石建造空间分布,总结了额尔古纳和松嫩地块之间新元古代—早石炭世洋—陆转换过程。

关键词: 洋—陆转换, 俯冲增生杂岩, 构造演化

Abstract: Aiming at the important scientific problem of the location and tectonic evolution of the northeast micro-block group in Northern China,based on the ocean-land conversion and continental dy⁃ namics theory,the types and tectonic environments of ophiolite in the erguna-Songnen block are identified by systematic analysis of the material composition of Xinlin-Tayuan-Xinglong subduction accretion com⁃ plex belt of Neoproterozoic to Early Cambrian and Nenjiang-Heihe subduction accretion complex belt of Early Carboniferous,and the types and tectonic setting of ophiolite in subduction accretion complex zone are identified.The study results show that:The ophiolite types of neoproterozoic Xinlin-Tayuan-Xinglong subduction accretion complex mainly include SSZ type ophiolite-niobium-rich basic volcanic rocks,mantle plume type ophiolite-ultramafic rock and gabbro assemblage,and ophiolite ultramafic rock and gabbro as⁃ semblage related to arc-basin evolution.The ophiolite type of the Nenjiang-Heihe subduction accretion complex in the Early Carboniferous is mainly composed of ultramafic and gabitic assemblages related to arc-basin evolution.Based on the material composition of Xinlin-Tayuan-Xinglong subduction accretion complex belt of Neoproterozoic and Early Cambrian,and the spatial distribution of magmatic arcs and re⁃ gional molasite formations of Nenjiang-Heihe subduction accretion complex belt of Early Carboniferous, the oceanic and continental transition process of Neoproterozoic and Early Carboniferous between Erguna Block and Songnen Block is summarized.

Key words: ocean-land transformation, subduction-accretionary complex, tectonic evolution