Petrographic and geochemical perspectives of the Azafrán Unit in the Río Blanco – La Esperanza section, Baños, Ecuador
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Keywords:
Azafrán, Petrography, Geochemistry, Dynamic Metamorphism, EcuadorAbstract
Previous investigations documented the best exposures of the Azafrán Unit in the Río Blanco–La Esperanza section; however, detailed information regarding its petrography, geochemistry, and the degree and type of metamorphism is lacking. The present study aims to characterize the
lithostratigraphy, petrography, geochemistry, and metamorphic grade of the Azafrán Unit in order to understand its geological and tectonic evolution. The research examines the lithological and metamorphic
variability observed in the field, evaluating its relationship with magmatic processes and tectonic deformation. Through detailed geological mapping, twelve representative samples of the Azafrán Unit were collected. The results indicate that the unit is composed of monzogranites,
schists, and gneisses, with phaneritic and granoblastic textures. Geochemical analyses reveal a high-K calc-alkaline affinity and enrichment in incompatible elements, indicating a magmatic origin associated with subduction processes. Metamorphism is characterized by greenschist facies, with temperature and pressure gradients ranging from 350 °C to
500 °C and from 3 to 8 kbar, respectively. In this context, the findings confirm that the metamorphosed granitoid series of the Azafrán Unit was subjected to dynamic tectono-metamorphic environments, where deformation and magmatism interacted within an active continental
margin framework. The identified structural heterogeneity rules out homogeneous metamorphic episodes and constitutes evidence of spatial and temporal variations in the intensity of tectonic and metamorphic events.
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