Journal of Structural Geology

Are viscosity ratios of rocks measurable from cleavage refraction?
pp. 895-901(7)
Authors: Yue R.-X.; Mao S.-S.; Treagus S.H.

Travitonics: using travertines in active fault studies
pp. 903-916(14)
Authors: Hancock P.L.; Chalmers R.M.L.; Altunel E.; Cakir Z.

Reversed structures and bounce structures: are they recognizable? Are they real?
pp. 917-921(5)
Author: Means W.D.

Strain compatibility and shear zones: is there a problem?
pp. 923-932(10)
Author: Hudleston P.

A fundamental problem with the kinematic interpretation of geological structures
pp. 933-937(5)
Authors: Jiang D.; Williams P.F.

The future of failure: stress or strain?
pp. 939-948(10)
Authors: Lloyd C.J.; Yong Z.; Watterson J.

Can field data constrain rock viscosities?
pp. 949-957(9)
Author: Talbot C.J.

Displacement control of geologic structures
pp. 959-967(9)
Authors: Tikoff B.; Wojtal S.F.

Fabric stability in oblique convergence and divergence
pp. 969-974(6)
Authors: Teyssier C.; Tikoff B.

Are S-C structures, duplexes and conjugate shear zones different manifestations of the same scale-invariant phenomenon?
pp. 975-984(10)
Author: Hippertt J.

Understanding the process of faulting: selected challenges and opportunities at the edge of the 21st century
pp. 985-993(9)
Author: Schultz R.A.

Do faults preserve a record of seismic slip? A field geologist's opinion
pp. 995-1001(7)
Author: Cowan D.S.

Fault death: a perspective from actively deforming regions
pp. 1003-1010(8)
Authors: Cheng K.F.; Hsueh H.M.; Jackson J.

Normal faults in thrust sheets: pre-orogenic extension, post-orogenic extension, or both? - European Association of Petroleum Geoscientists Special Publication
pp. 1011-1018(8)
Author: Tavarnelli E.

Fault relays, bends and branch-lines
pp. 1019-1026(8)
Authors: Walsh J.J.; Watterson J.; Bailey W.R.; Childs C.

Normal fault corrugation: implications for growth and seismicity of active normal faults
pp. 1027-1038(12)
Authors: Best D.J.; Rayner J.C.W.; Ferrill D.A.; Stamatakos J.A.; Sims D.

Clay gouge
pp. 1039-1048(10)
Authors: Vrolijk P.; van der Pluijm B.A.

Transitional-tensile fracture propagation: a status report
pp. 1049-1055(7)
Author: Engelder T.

Strain and stress
pp. 1057-1063(7)
Authors: Kutoyants Y.A.; Spokoiny V.; Marrett R.; Peacock D.C.P.

Stress, strain and fault patterns
pp. 1065-1070(6)
Authors: Husler J.; Nieto-Samaniego A.F.

Can we understand structural and tectonic processes and their products without appeal to a complete mechanics?
pp. 1071-1088(18)
Authors: Fletcher R.C.; Pollard D.D.

Strain, displacement and rotation associated with the formation of curvature in fold belts; the example of the Jura arc
pp. 1089-1101(13)
Authors: Devroye L.; Krzyzak A.; Hindle D.; Burkhard M.

Large-scale coast-parallel displacements in the Cordillera: a granitic resolution to a paleomagnetic dilemma
pp. 1103-1108(6)
Authors: Liang T.; Johnston S.T.

Translation and the resolution of the pluton space problem
pp. 1109-1117(9)
Authors: Tikoff B.; de Saint Blanquat M.; Teyssier C.

Re-examining Argand's view of the Siviez-Mischabel nappe
pp. 1119-1124(6)
Authors: Markley M.J.; Teyssier C.; Caby R.

Should felsic magmas be considered as tectonic objects, just like faults or folds?
pp. 1125-1130(6)
Author: Vigneresse J.-L.

Is there a close spatial relationship between faults and plutons?
pp. 1131-1142(12)
Authors: Paterson S.R.; Schmidt K.L.

Pluton accommodation at high strain rates in the upper continental crust. The example of the Central Extremadura batholith, Spain
pp. 1143-1149(7)
Authors: Fernandez C.; Castro A.

Ramifications of four-dimensional progressive deformation in contractional mountain belts
pp. 1151-1160(10)
Authors: Gray M.B.; Mitra G.

In defense of magmatic diapirs
pp. 1161-1173(13)
Authors: Miller R.B.; Paterson S.R.

Deformation style way back when: thoughts on the contrasts between Archean/Paleoproterozoic and contemporary orogens
pp. 1175-1182(8)
Author: Marshak S.

Near-orthogonal foliation development in orogens: meaningless complexity, or reflection of fundamental dynamic processes?
pp. 1183-1187(5)
Author: Johnson S.E.

How pressure solution creep and fracturing processes interact in the upper crust to make it behave in both a brittle and viscous manner
pp. 1189-1197(9)
Authors: Gratier J.-P.; Renard F.; Labaume P.

`Crack-seal', slip: a new fault valve mechanism?
pp. 1199-1207(9)
Authors: Petit J.-P.J.-P.; Wibberley C.A.J.; Ruiz G.

Competitive macroscopic deformation processes
pp. 1209-1218(10)
Author: Woodward N.B.

Are feldspar-to-mica reactions necessarily reaction-softening processes in fault zones?
pp. 1219-1227(9)
Authors: Bobkov S.G.; Houdre C.; Wibberley C.

Fluid inclusions: tectonic indicators
pp. 1229-1235(7)
Author: Boullier A.-M.

Are fluid inclusion planes useful in structural geology?
pp. 1237-1243(7)
Author: Lespinasse M.

Construction and systematic assessment of relative deformation histories
pp. 1245-1253(9)
Authors: Potts G.J.; Reddy S.M.

Constraining absolute deformation ages: the relationship between deformation mechanisms and isotope systematics
pp. 1255-1265(11)
Authors: Reddy S.M.; Potts G.J.

How successful are analogue models in addressing the influence of pre-existing fabrics on rift structure?
pp. 1267-1274(8)
Author: Morley C.K.