It is generally accepted that grain boundary sliding (GBS) is the dominant deformation
mechanism in fine-grained strain localization zones. However, the lifetime of GBS during …

古地理学是一门强数据依赖性学科, 古地理重建作为古地理学的核心任务之一,
着眼于研究地质历史时期地球表面的地理, 生物, 气候面貌及其演化规律 …

Dolomitic marble on the island of Naxos was deformed at variable temperatures ranging
from 390° C to> 700° C. Microstructural investigations indicate two end-member of …

To explore the rheology of dolomite and investigate recent findings regarding the so‐called
inversion of activation energy between dislocation and diffusion creep, we compressed …

Calcite and dolomite are the two most common minerals in carbonate-bearing faults and
shear zones. Motivated by field examples from exhumed seismogenic faults in the Italian …

A fabric study of forsterite marble and calc-silicate rock paragenetic minerals is presented for
samples collected in the Almadén de la Plata massif of SW Spain, that experienced Variscan …

We compare microstructures and lattice preferred orientations (LPO) in shear zones formed
in two experimentally deformed and two naturally deformed dolomites. Experimental …

Paleogeography is a typical data-reliable subject. Paleogeographic reconstruction focuses
on the characteristics of geographic, life, and climate changes on the Earth's surface through …

Abstract Intermediate depth (170-400 km) deep focus earthquakes are observed in
subducting slabs, but unlike shallow (50-170 km) and deep (400-660 km) deep focus …

While Earth's crust is often modelled as a homogenous material, heterogeneities such as
foliations, lattice preferred orientations (LPOs), and pre-existing brittle deformations are …