Mineral paragenesis and metamorphic evolution of geological formations in the Loango sector, Province of Central Kongo, Democratic Republic of the Congo

Authors

  • Emmanuel Manteko Matondo Centre de Recherche Géologiques et Minières (CRGM), Kinshasa, République Démocratique du Congo Author
  • Ciceron Nteme Mpio Centre de Recherche Géologiques et Minières (CRGM), Kinshasa, République Démocratique du Congo Author
  • Michel Okondo Nkoso Centre de Recherche Géologiques et Minières (CRGM), Kinshasa, République Démocratique du Congo Author
  • Ange Gabriel Makaya Lutua Centre de Recherche Géologiques et Minières (CRGM), Kinshasa, République Démocratique du Congo Author
  • Steeve Musianga Siyum Centre National de Télédétection (CNT), Kinshasa, République Démocratique du Congo Author
  • Labem Ndumba Dadou Centre National de Télédétection (CNT), Kinshasa, République Démocratique du Congo Author
  • Djodjo Kra Centre de Recherche Géologiques et Minières (CRGM), Kinshasa, République Démocratique du Congo Author
  • Bertin Dingadia Wasamba Centre de Recherche en Eau et Environnement (CREE), Kinshasa, République Démocratique du Congo Author
  • Carlos Samuel Mbokama Mwana Centre National de Télédétection (CNT), Kinshasa, République Démocratique du Congo Author

DOI:

https://doi.org/10.59228/rcst.024.v3.i4.118

Keywords:

Geological formation, petrographic, mineralogy, metamorphism, lithofacies

Abstract

The aim of this work is to characterize the mineralogical assemblages of the rocks encountered in the Loango sector, with a view to determining the degree of metamorphism they have undergone, and to enrich and supplement the information essential for the geological mapping of the Central Kongo province. Specifically, we wanted to know whether the geological formations in the Loango area had petrographic characteristics that would enable us to classify them. We carried out a field trip and collected seven rock samples. After macroscopic and microscopic description in the CRGM laboratory, four lithofacies were determined: sericite schists, quartzophyllades, amphibolites and biotitoschists. This enabled us to classify the rocks according to metamorphic facies. The study of mineral paragenesis in the study area points to a regional metamorphism transiting from the epizone to the mesozone, characterized by the presence of sericite and biotite. 

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Published

2024-12-31

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