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Member Since 1981
Philip C. England
Retired
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Shear heating and the metamorphic record of subduction metamorphism: recognition and implications
FROM MICRONS TO MOUNTAINS: METAMORPHIC RECORDS OF HEAT AND MASS TRANSFER III ORAL
volcanology, geochemistry and petrology | 10 december 2024
Simon R. Wallis, Philip C. England, Takumi Matsumo...
Analysis of dense heat flow data from the forearc region of NE Japan reveals significant shear heating along the subduction boundary and suggests temp...
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Implications of Surface Heat Flux for Shear Stress and Temperature on the Plate Interface Beneath Northern Honshu
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
07 february 2024
Philip C. England, Takumi Matsumoto, Simon R. Wall...

Measurements of surface heat flux from boreholes of the NIED Hi‐net network of seismometers are used to determine temperature and shear stres...

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Metamorphism and Deformation on Subduction Interfaces: 1. Physical Framework
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
05 january 2023
Philip C. England, Andrew Smye

A thermal and mechanical framework is presented for analysis of pressure‐temperature (P‐T) data and structural observations from high&#...

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Metamorphism and Deformation on Subduction Interfaces: 2. Petrological and Tectonic Implications
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
05 january 2023
Andrew Smye, Philip C. England

The compositional range of ∼2,000 marine sediments and ∼19,000 oceanic igneous rocks is encapsulated by a set of 12 sedimentary and 10 ...

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Changes in Plate Motions Caused by Increases in Gravitational Potential Energy of Mountain Belts
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
10 october 2022
Philip C. England, Peter H. Molnar

Reconstructions of motions of the Nazca, South American, and Indian plates record short‐duration (≲10 Myr) variations in angular v...

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Petrological and Tectonic Implications of Dissipative Heating on Subduction Interfaces
SUBDUCTION TOP TO BOTTOM: FOCUS ON THE FOREARC IV ORAL
tectonophysics | 14 december 2021
Andrew Smye, Philip C. England
Shear heating controls the metamorphic grade, dehydration, melting and strength of subduction interfaces. Here, we use an established thermal and mech...
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The Global Range of Temperatures on Convergent Plate Interfaces
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
20 august 2021
Philip C. England, Dave May

We present accurate analytical expressions for temperatures on the upper parts of convergent plate boundaries where there are rigid plates both abo...

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Geomorphology and Paleoseismology of the Weinan Fault, Shaanxi, Central China, and the Source of the 1556 Huaxian Earthquake
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
08 december 2020
Xijie Feng, Ji Ma, Yu Zhou, Philip C. England, Bar...

The 1556 CE Huaxian earthquake resulted in an estimated 830,000 deaths and caused widespread devastation in the Weihe Basin, China. Seismic in...

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