12.2 Paragenetic Sequences and Diagrams

Paragenetic sequences and diagrams are crucial tools for understanding mineral formation and alteration over time. They reveal the order of mineral growth, providing insights into geological conditions and processes that shaped rocks and ore deposits.

These tools help geologists reconstruct complex geological histories, determine timing of mineralization events, and interpret textural relationships between minerals. They're essential for economic geology, guiding exploration strategies and unraveling the evolution of ore-forming systems.

Paragenesis: Mineral Formation and Alteration

Concept and Significance

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  Vein Mineralogy and Hydrothermal Gold Mineralization at the Kyaw Soe Thu Prospect in the Wabo ... View original

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  Putting It Together: Rocks and the Rock Cycle | Geology View original

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  Vein Mineralogy and Hydrothermal Gold Mineralization at the Kyaw Soe Thu Prospect in the Wabo ... View original

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• Paragenesis describes the sequence of mineral formation and alteration events in rocks or ore deposits over time
• Provides crucial information about geological conditions and processes leading to mineral formation in a specific order
• Helps geologists understand the evolution of mineral assemblages and changing environmental conditions during rock formation
• Essential for unraveling complex geological histories and determining the timing of mineralization events
• Particularly important in economic geology for understanding ore deposit formation and identifying potential exploration targets (porphyry copper deposits)
• Reveals information about temperature, pressure, and chemical conditions during mineral formation and subsequent alteration processes
• Fundamental to interpreting textural relationships between minerals and understanding their genetic associations

Applications in Geological Analysis

• Used to reconstruct the geological history of a rock or deposit
• Aids in identifying different stages of mineral growth and alteration (metamorphic reactions)
• Helps determine the relative timing of geological events (intrusion of igneous bodies)
• Supports the interpretation of fluid-rock interactions and their effects on mineral assemblages
• Assists in understanding the evolution of ore-forming systems over time (epithermal gold deposits)
• Contributes to the development of genetic models for mineral deposits
• Guides exploration strategies by predicting the spatial and temporal distribution of minerals

Paragenetic Diagrams: Sequence of Events

Construction and Components

• Graphical representations of the order and timing of mineral formation and alteration in rocks or deposits
• Use horizontal bars to represent the duration of mineral growth or stability, with time progressing from left to right
• Vertical axis lists minerals present, often grouped by genetic associations or mineral classes
• Overlapping bars indicate contemporaneous mineral formation
• Gaps may represent periods of dissolution or non-deposition
• Often include additional information such as temperature ranges, deformation events, or fluid composition changes
• Construction involves careful observation of mineral textures, crosscutting relationships, and geochemical analysis

Interpretation and Analysis

• Requires understanding of mineral stability fields, reaction kinetics, and principles of crystal growth and dissolution
• Allows visualization of the temporal relationships between different minerals and geological events
• Helps identify periods of mineral growth, alteration, and stability
• Reveals patterns of mineral succession and replacement
• Assists in recognizing episodic or continuous mineralization processes
• Supports the identification of different stages in the evolution of a rock or deposit (prograde and retrograde metamorphism)
• Facilitates comparison of paragenetic sequences between different parts of a deposit or between different deposits

Crosscutting Relationships: Timing of Formation

Principles and Indicators

• Crosscutting relationships occur when one mineral or structure cuts across another, indicating earlier formation of the crosscut feature
• Overgrowths are newer mineral layers forming on pre-existing mineral grains, providing evidence of multiple growth stages
• Principle of superposition applies to mineral growth, with younger mineral layers typically forming on top of older ones in undisturbed sequences
• Mineral veins cutting through host rocks or other mineral assemblages indicate later formation relative to the material they crosscut
• Reaction rims or coronas around mineral grains suggest later alteration or metamorphic events affecting pre-existing minerals
• Inclusions of one mineral within another generally indicate earlier formation of the included mineral

Analytical Techniques

• Careful examination of grain boundaries and crystal faces can reveal evidence of mineral replacement or pseudomorphism
• Microscopic analysis of thin sections helps identify fine-scale crosscutting relationships and mineral textures
• Cathodoluminescence imaging can reveal growth zoning and multiple generations of minerals (quartz, calcite)
• Electron microprobe analysis allows for detailed chemical mapping of mineral grains and identification of compositional zoning
• Isotope geochemistry can provide absolute age constraints on mineral formation and alteration events
• Fluid inclusion studies help determine the conditions of mineral formation and identify different generations of fluids
• Integration of multiple analytical techniques improves the accuracy of paragenetic interpretations

Paragenetic Sequences: Geological History

Reconstruction Methods

• Provide a chronological framework for understanding the evolution of a rock or deposit over geological time
• Analysis of mineral assemblages and textural relationships reveals changes in temperature, pressure, and fluid composition during rock formation
• Presence of index minerals or mineral associations helps constrain pressure-temperature conditions at different stages of rock history
• Identification of hydrothermal alteration patterns indicates fluid flow events and their timing relative to primary mineralization
• Recognition of multiple generations of the same mineral provides insights into repeated or cyclical geological processes (quartz veining events)
• Integration of paragenetic data with other geological and geochemical information allows for comprehensive reconstruction of deposit formation history
• Distinguishes between primary depositional features and later diagenetic or metamorphic overprints in sedimentary and metamorphic rocks

Implications and Applications

• Helps establish the relative timing of mineralization events in complex ore systems
• Aids in understanding the evolution of fluid chemistry and its impact on mineral precipitation (evolution of porphyry systems)
• Supports the development of genetic models for different types of mineral deposits
• Guides exploration strategies by predicting the spatial distribution of ore minerals
• Assists in unraveling the tectonic and metamorphic history of rock units
• Contributes to the understanding of basin evolution and diagenetic processes in sedimentary rocks
• Supports the interpretation of geochronological data by providing a relative time framework