This thesis reports on a research into the progressive development of fibrous aggregates, e.g. calcite, quartz and mica crystals in veins and strain fringes. The study is based on microstructural analysis of natural examples and on computer experiments. Investigation of fibrous looking elongate crystals in striped bedding-veins from the Orobic Alps, Italy indicate that these crystals do not track the opening trajectory of the veins but are oriented at an angle of up to 80° to the opening direction. Microstructural analysis of quartz, calcite and chlorite fibres in antitaxial strain fringes indicate that most strain fringes contain complex intergrowth of tracking (displacement-controlled) and non-tracking (face-controlled) fibres. To explain...
Deformed strain fringes in iron formation rocks show complex quartz fiber patterns that grew alongsi...
The experiments described are a continuation of a series of tests on Solnhofen limestone, Carrara ma...
In order to use intracrystalline deformation structures in quartz as palaeopiezometer and as indicat...
This thesis reports on a research into the progressive development of fibrous aggregates, e.g. calci...
Abslnlct-Detailed obscrvationsof a set of fibrous antitaxial calcite veins in a slate reveal that so...
Abstract--Detaded observations of a set of fibrous antitaxial calcite veins in a slate reveal that s...
We developed two programs, "Vein Growth" and "Fringe Growth", to investigate progressive growth of c...
Antitaxial non-deforming strain fringes from Lourdes, France, show complex quartz, calcite and chlor...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
Veins occurring at the edge of the dextral Indian Islands Fault (Newfoundland) are folded in respons...
Folds with hinge lines subparallel to stretching lineation are common features in shear zones and re...
The textures of synkinematic veins involve a complex interplay of crystal growth and deformation. Qu...
The geometry, microtextures, and c-axis fabrics of calcite “beef” veins in the Lower Jurassic black ...
Fibrous mineral veins are extremely important structures in mudrocks because they represent phases ...
The development of fibrous morphology and capability of fibres for tracking the opening trajectory w...
Deformed strain fringes in iron formation rocks show complex quartz fiber patterns that grew alongsi...
The experiments described are a continuation of a series of tests on Solnhofen limestone, Carrara ma...
In order to use intracrystalline deformation structures in quartz as palaeopiezometer and as indicat...
This thesis reports on a research into the progressive development of fibrous aggregates, e.g. calci...
Abslnlct-Detailed obscrvationsof a set of fibrous antitaxial calcite veins in a slate reveal that so...
Abstract--Detaded observations of a set of fibrous antitaxial calcite veins in a slate reveal that s...
We developed two programs, "Vein Growth" and "Fringe Growth", to investigate progressive growth of c...
Antitaxial non-deforming strain fringes from Lourdes, France, show complex quartz, calcite and chlor...
The microstructure and crystallographic preferred orientation (CPO) of quartz were quantified in 17 ...
Veins occurring at the edge of the dextral Indian Islands Fault (Newfoundland) are folded in respons...
Folds with hinge lines subparallel to stretching lineation are common features in shear zones and re...
The textures of synkinematic veins involve a complex interplay of crystal growth and deformation. Qu...
The geometry, microtextures, and c-axis fabrics of calcite “beef” veins in the Lower Jurassic black ...
Fibrous mineral veins are extremely important structures in mudrocks because they represent phases ...
The development of fibrous morphology and capability of fibres for tracking the opening trajectory w...
Deformed strain fringes in iron formation rocks show complex quartz fiber patterns that grew alongsi...
The experiments described are a continuation of a series of tests on Solnhofen limestone, Carrara ma...
In order to use intracrystalline deformation structures in quartz as palaeopiezometer and as indicat...