Introduction
Stable isotopes have emerged as essential tools in understanding ore-forming processes and the genesis of mineral deposits. By analyzing the isotopic composition of elements such as oxygen, carbon, and sulfur within ore minerals and surrounding geological matrices, researchers can decipher the physicochemical conditions prevalent during formation. This article delves into the application of stable isotope geochemistry in tracing the origins, transport mechanisms, and depositional environments of mineral resources. Through a detailed examination of case studies and methodologies, we aim to illuminate the intricacies of stable isotope behavior and it’s implications for economic geology and exploration strategies.
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