Abstract

AbstractBuilding on recent developments in phase‐field modeling of structural diagenesis, we present an analysis of single‐seal syntaxial calcite vein microstructure in a variety of limestones. We focus on the effects of fracture aperture, intergranular versus transgranular fracturing, crystal habit and the presence of second phases in the host rock, to systematically investigate a simplified set of models covering the main classes of limestone in 2D. We incorporate the kinematic process of growth competition between differently oriented crystals, growth rate anisotropy between rough and faceted crystal surfaces and different growth rates on intergranular to transgranular fractures. Results show that within the considered parameter space we can reproduce a wide range of vein microstructures in limestone known in nature, such as stretched crystals, wide‐blocky veins, and elongated crystals. We identify five archetypes of vein microstructures in limestones, which are diagnostic for different kinematics and evolution of transport processes and illustrate the effect of key parameters in microstructure maps. We show how syntaxial veins with median line form after intergranular fracturing, while stretched crystals indicate transgranular fracturing. Intergranular fracturing leads to stronger growth competition and more prominent CPO in syntaxial veins. Our results can be extended to 3D to include multiple crack‐seal events, pore‐space cementation and simulation of fluid flow, providing a generic platform for modeling structural diagenesis in limestones.

Highlights

  • The chemistry and mechanics of fracture sealing in deforming hydrothermal and reactive environments is important in basic geoscience and applied studies

  • Building on recent developments in phase-field modeling of structural diagenesis, we present an analysis of single-seal syntaxial calcite vein microstructure in a variety of limestones

  • We focus on the effects of fracture aperture, intergranular versus transgranular fracturing, crystal habit and the presence of second phases in the host rock, to systematically investigate a simplified set of models covering the main classes of limestone in 2D

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Summary

Introduction

The chemistry and mechanics of fracture sealing in deforming hydrothermal and reactive environments is important in basic geoscience and applied studies. Syntectonic syntaxial calcite or quartz veins are ubiquitous in rocks at low metamorphic grades in the upper and middle crust (Passchier & Trouw, 2005; Ramsay & Huber, 1983). The formation of these veins includes multiple coupled mechanical, hydraulic, SPÄTH ET AL. The evolution of vein microstructures (Durney, 1973; Passchier & Trouw, 2005; Ramsay & Huber, 1983) remains an open field (e.g., influence of fracture type)

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