Petrography and geochemistry of Late Carboniferous dolostone-hosted soapstone in the Sherwan Formation, Hazara Basin: insights into hydrothermal and dynamic metamorphic processes
Year: 2025
Type: article
Abstract: Introduction This study investigates the petrography and geochemistry of soapstone-bearing dolomite within the Sherwan Formation, Hazara Basin, with a focus on understanding hydrothermal dynamic metamorphism and resolving the age controversy surrounding the host rock. Methods Field observations, petrographic analysis, and geochemical techniques were used, including X-ray diffraction (XRD), scanning electron microscopy (SEM), and energy-dispersive spectroscopy (EDS), to characterize mineral composition and alteration processes. Results Petrographic evidence confirms that talc formed through hydrothermal alteration of Late Carboniferous dolomite, facilitated by faulting, folding, and silica-rich fluid infiltration. Distinct geological features such as stromatolitic dolomite, pseudotachylitic veins, and mylonitization suggest episodic brittle deformation under high-temperature conditions. The presence of Anthracoporella spectabilis supports a Late Carboniferous age for the dolomite, while the soapstone is dated to the Permian, linked to Pre-Himalayan tectonics, Panjal volcanism, and dolerite intrusions. Mineralogical analyses reveal that soapstone is primarily composed of talc (steatite), with secondary minerals including brucite, magnesite, willemseite, and montmorillonite. The occurrence of pyrite and hematite indicates hydrothermal interactions, contributing to metal enrichment and oxidation. Discussion Geochemical data show silica enrichment and structural weakening as key factors in dolomite-to-talc transformation. Trace levels of chromium (100–300 ppm) raise concerns over Cr6+ toxicity, but the absence of arsenic, lead, cadmium, and mercury supports the environmental safety and industrial potential of the soapstone. The study underscores the complex interplay of tectonic, metamorphic, and geochemical processes in the evolution of the Sherwan soapstone.
Source: Frontiers in Earth Science
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: gold
Estimated APC paid: $3,801
OpenAlex ID: W4410617314