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Deeply buried basinal brines are heated, lowering the kinetic barrier for magnesium hydration. These fluids travel upward along faults, dolomitizing adjacent limestones. 5. Classification Matrix for Carbonate Rocks

| Topic | Source | Key Content | | :--- | :--- | :--- | | | Semantic Scholar | Investigates the debated origin of fine-grained carbonate mud, crucial for understanding ancient carbonate sequences. | | Sedimentology and Geochemistry of Dolostones | Semantic Scholar | Addresses the long-standing "dolomite problem" and the origin of this enigmatic mineral. | | Origin of Primary and Diagenetic Carbonates (Eocene Green River Formation) | USGS Publications Warehouse | A classic USGS study on lacustrine carbonates, providing a high-quality, free PDF case study. | | Quantitative Diagenesis of Carbonate Reservoir Rocks | Imperial College London (Spiral) | A modern paper (2022) detailing quantitative methods to study diagenesis and its effect on porosity, offering cutting-edge methodology. | | Computer Modeling of Carbonate Platforms | Kansas Geological Survey | A resource for understanding the large-scale modeling of carbonate platform depositional systems. |

Soon, life joined the party. Microscopic algae and cyanobacteria began building stromatolites origin of carbonate sedimentary rocks pdf extra quality

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These are the cornerstone resources, offering systematic, textbook-level coverage of the entire subject. Deeply buried basinal brines are heated, lowering the

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Review like stable isotope geochemistry ( ) and cathodoluminescence. Classification Matrix for Carbonate Rocks | Topic |

┌───────────────────────────┐ │ DIAGENETIC ENVIRONMENTS │ └─────────────┬─────────────┘ │ ┌────────────────────────┼────────────────────────┐ ▼ ▼ ▼ ┌─────────────────┐ ┌─────────────────┐ ┌─────────────────┐ │ METEORIC │ │ MARINE │ │ DEEP BURIAL │ ├─────────────────┤ ├─────────────────┤ ├─────────────────┤ │ • Fresh water │ │ • Marine fluids │ │ • High pressure │ │ • Dissolution │ │ • Cementation │ │ • Compaction │ │ • Lithification │ │ • Micritization │ │ • Stylolites │ └─────────────────┘ └─────────────────┘ └─────────────────┘ The Dolomite Problem

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