Reference health

The role of microcracking in shear-fracture propagation in granite

https://doi.org/10.1016/0191-8141(94)e0018-t
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35/35 checkable references clean · checked 2026-07-23

Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a retraction, withdrawal, or removal notice.

9 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.

The 35 checked references that resolve
resolves10.1016/0001-6160(86)90086-6
The failure of brittle solids containing small cracks under compressive stress states
resolves10.1007/BF00878002
The damage mechanics of brittle solids in compression
resolves10.1029/GL012i009p00557
Sawtooth segmentation and deformation processes on the southern San Andreas Fault, California
resolves10.2475/ajs.248.6.378
Composition of the granites of Westerly and Bradford, Rhode Island
resolves10.2475/ajs.248.1.22
On a distinction between late-magmatic and post-ma gmatic replacement reactions
resolves10.1016/0191-8141(88)90019-3
On the formation and growth of faults: an experimental study
resolves10.1680/geot.1969.19.3.376
Anisotropy of Granites: A Reflection of Microscopic Fabric
resolves10.1029/JB091iB12p12743
Micromechanics of thermally induced cracking in three crustal rocks
resolves10.1029/JB095iB13p21613
Mechanical anisotropy of gneiss: Failure criterion and textural sources of directional behavior
resolves10.1029/TC004i007p00721
Origin, damping, and pattern of development of faults in granite
resolves10.1029/JB081i020p03484
Comparison of calculated and observed crack densities and seismic velocities in westerly granite
resolves10.1029/JB090iB04p03105
Compression‐induced microcrack growth in brittle solids: Axial splitting and shear failure
resolves10.1016/0148-9062(87)90177-X
The effect of pre-existing microcavities on mechanical rock performance in sedimentary and crystalline rocks
resolves10.1111/j.1365-246X.1984.tb02229.x
The evolution of a thrust fault system: processes of rupture initiation, propagation and termination in the 1980 El Asnam (Algeria) earthquake
resolves10.1016/0148-9062(79)90772-1
Crack growth and development during creep of Barre granite
resolves10.1016/0040-1951(83)90198-1
Microcracks in rocks: A review
resolves10.1029/JB095iB12p19257
Basal slip and mechanical anisotropy of biotite
resolves10.1029/92JB01828
Room temperature creep in saturated granite
resolves10.1038/350039a0
Quasi-static fault growth and shear fracture energy in granite
resolves10.1029/91JB01642
A multiple‐crack model of brittle fracture: 1. Non‐time‐dependent simulations
resolves10.1029/JB088iB01p00585
Microcrack connectivity in rocks: A renormalization group approach to the critical phenomena of conduction and failure in crystalline rocks
resolves10.3133/ofr93245
Microcrack populations associated with a propagating shear fracture in granite
resolves10.3133/ofr87279
Fluid-rock interaction and fracture development in "crystalline" rock types
resolves10.3133/ofr90349
Faults, fractures, and other deformation features produced during loading of granite in triaxial equipment
resolves10.1130/0016-7606(1958)69[465:EDAFIW]2.0.CO;2
EXPERIMENTAL DEFORMATION AND FAULTING IN WOMBEYAN MARBLE
resolves10.1016/0148-9062(72)90050-2
Crack growth and faulting in cylindrical specimens of chelmsford granite
resolves10.1029/JB088iB01p00555
Nucleation and growth of strike slip faults in granite
resolves10.2475/ajs.275.3.318
Toward a quantitative relationship between elastic properties and cracks in low porosity rocks
resolves10.1016/0148-9062(74)92874-5
Direct observation of microcavities in crystalline rocks
resolves10.1126/science.205.4405.495
Microcracking and Healing in Granites: New Evidence from Cathodoluminescence
resolves10.1016/0148-9062(76)91937-9
Development of stress-induced microcracks in Westerly Granite
resolves10.1029/JB082i036p05705
Experimental deformation of dry westerly granite
resolves10.1016/0148-9062(82)91631-X
Micromechanics of faulting in westerly granite
resolves10.1029/JB087iB02p00990
Shear fracture energy of Westerly granite from post‐failure behavior
resolves10.1016/0167-6636(85)90023-7
Geometric probability approach to the characterization and analysis of microcracking in rocks
The 9 references without a DOI — listed, not checked
no DOI — not checked10.1016/0191-8141(94)E0018-T_BIB3
no DOI — not checkedSlip distribution and oblique segments of the San Andreas fault, California: observations and theory
no DOI — not checkedThe Commercial Granites of New England
no DOI — not checkedJoints and shear fractures in rock
no DOI — not checkedStrain energy density factor: A potential fracture mechanics fault propagation criterion
no DOI — not checkedObservations of quasi-static fault growth from acoustic emissions
no DOI — not checkedMicrocrack interaction leading to shear fracture
no DOI — not checkedTheoretical displacements and stresses near fractures in rock: with application to faults, joints, veins, dikes, and solution surfaces
no DOI — not checked10.1016/0191-8141(94)E0018-T_BIB35
What this badge says. CiteStamped means the CHECKABLE references of this work were clean at the dated check: each resolved to a known work in a public registry, and none carried a retraction notice at that time. It says nothing about the quality, findings, or importance of the work itself, and nothing about references deposited without a DOI.

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