CÁC THÀNH TẠO PHUN TRÀO VÀ XÂM NHẬP MESOZOI MUỘN TUYẾN A LƯỚI - ĐẮK RÔNG

Lê Tiến Dũng, Phạm Thị Vân Anh, Tô Xuân Bản
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Authors

  • Lê Tiến Dũng
  • Phạm Thị Vân Anh
  • Tô Xuân Bản

DOI:

https://doi.org/10.15625/0866-7187/27/2/9403

Abstract

Dackrong-Aluoi Volcanic line, West of Quang Tri and Thua Thien-Hue provinces, includes basalt, andesite, dacite, riolite and granite-porphyritic granophyritic shallow intrusive rocks.

According to geological and petrological characteristics, they belong to effusive-explosivefacie, truly volcanic and hypabyssall facie o ffracture type of early Cretaceous age.

In chemical aspect, the rocks form high potassium calc-alkal ine series in the activecontinental margin of Andes Type.

Volcanic suffered strong hydrothermal metamorphosed profilitisation, bersitisation and argilitisation that related to silver-gold and polymetal mineralization.

Small intrusive bodies and light color porphyritic granite Dikes which are strongly weathered, related to kaolinite deposits with high quality and medium size.

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Published

27-03-2017

How to Cite

Dũng, L. T., Anh, P. T. V., & Bản, T. X. (2017). CÁC THÀNH TẠO PHUN TRÀO VÀ XÂM NHẬP MESOZOI MUỘN TUYẾN A LƯỚI - ĐẮK RÔNG. Vietnam Journal of Earth Sciences, 27(2), 133–141. https://doi.org/10.15625/0866-7187/27/2/9403

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Articles