ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
紫金山岩体的热力构造类型、期次及其对鄂尔多斯盆地东缘多种能源矿产的影响作用
  
关键词:Zijinshan rock body  thermal structure  energy resources and mineral  effect
基金项目:科技部国家重点基础研究(973项目)子课题(编号:2003CB214601-03C)
作者单位E-mail
杨永恒 中国地质大学能源学院,北京100083 yangyongheng2003@163.com 
杨兴科 长安大学地球科学与国土资源学院,陕西西安710054  
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摘要:
Thermal Structure Types and Stages of Zijinshan Rock Body and Their Influence upon Several Energy Resources and Minerals in Eastern Ordos Basin
      Zijinshan complex in eastern Ordos basin, an alkaline rock body formed in several stages, can be divided into six phases from the outer part to the core. The rock body morphologically forms a normal dome type thermal structure. Monzonite, aegirine-augite syenite, malignite and nepheline syenite belong to the intermediate-deep intrusion type thermal structure, whereas phonolite/phonolitic volcanic breccia and trachyte/trachytic volcanic breccia are of the superficial/shallow volcanic eruption type. Since the beginning of Triassic period, there have occurred three thermal activities in Zijinshan area. The intermediate-deep intrusion from Late Jurassic to Early Cretaceous accelerated coal metamorphism which resulted in secondary hydrocarbon production. It also accelerated the maturity of Upper Paleozoic hydrocarbon source rock (coal and dark mudstone), and led to volcanic piercing closure resulting from upward magmatic intrusion, which finally became an oil/gas-bearing structure.
YANG Yong-heng,YANG Xing-ke.2007.Thermal Structure Types and Stages of Zijinshan Rock Body and Their Influence upon Several Energy Resources and Minerals in Eastern Ordos Basin[J].Acta Geoscientica Sinica,28(6):620-626.
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