Sheng Fan
www.shengfan-geology.com
0000-0002-0404-1374
University of Cambridge
20 papers found
Refreshing results…
Grain growth of natural and synthetic ice at 0 ºC
Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica
Using Misorientation and Weighted Burgers Vector Statistics to Understand Intragranular Boundary Development and Grain Boundary Formation at High Temperatures
Using misorientation and weighted Burgers vector statistics to understand the intragranular boundary development and grain boundary formation at high temperatures
Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz
Crystallographic Preferred Orientation (CPO) Development Governs Strain Weakening in Ice: Insights From High‐Temperature Deformation Experiments
Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica
Kinking facilitates grain nucleation and modifies crystallographic preferred orientations during high-stress ice deformation
Crystallographic preferred orientation (CPO) development governs the strain weakening in minerals with strong viscous anisotropy at high homologous temperatures (≥ 0.9): insights from up-strain ice deformation experiments
The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice
Full crystallographic orientation (<i>c</i> and <i>a</i> axes) of warm, coarse-grained ice in a shear-dominated setting: a case study, Storglaciären, Sweden
Using Grain Boundary Irregularity to Quantify Dynamic Recrystallization in Ice
Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C
Shallow seismic reflection imaging of the Alpine Fault through late Quaternary sedimentary units at Whataroa, New Zealand
Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics
Response to Reviewer 2
Response to Reviewer 1
Electron backscatter diffraction (EBSD) based determination of crystallographic preferred orientation (CPO) in warm, coarse-grained ice: a case study, Storglaciären, Sweden
Supplementary material to "Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C"
Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures
Missing publications? Search for publications with a matching author name.