Thermobarogeochemical model of deep fluid’s evolution in the Earth’s lithosphere
DOI:
https://doi.org/10.24028/gj.v47i2.322553Keywords:
fluid, inclusion, mineral, thermobarogeochemistry, model, lithosphereAbstract
A thermobarogeochemical model of the evolution of deep fluids in the Earth’s lithosphere (tectonosphere) was created, the main postulates of which is substantiated by the data of thermobarogeochemistry — the fundamental science on fluid inclusions as naturally preserved relics of the fluid mineral ore-oil-forming environment, the determinacy of which follows from the undeniable fact of their occlusion by microinclusions in crystals and preservation from the time of capture to the present. Analysis showed the real possibility of using inclusions to assess the fluid saturation of the subsoil and predict the ore-bearing and hydrocarbon saturation of promising structures. Supplementing the existing geological-geophysical and mineralogical-geochemical models with original data of the evolutionary model will form the basis of the Earth’s thermobarogeochemical model.
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