A coesite inclusion in dolomite in Dabie Shan, China: Petrological and rheological significance
about
First direct evidence of sedimentary carbonate recycling in subduction-related xenoliths.Ultrahigh-pressure metamorphism in the magnesite + aragonite stability field: evidence from two impure marbles from the Dabie-Sulu UHPM beltImpure marbles from the UHP Brossasco-Isasca Unit (Dora-Maira Massif, western Alps): evidence for Alpine equilibration in the diamond stability field and evaluation of the X(CO2) fluid evolution
P2860
A coesite inclusion in dolomite in Dabie Shan, China: Petrological and rheological significance
description
article
@en
im November 1994 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 1994
@uk
ലേഖനം
@ml
name
A coesite inclusion in dolomit ...... l and rheological significance
@en
A coesite inclusion in dolomit ...... l and rheological significance
@nl
type
label
A coesite inclusion in dolomit ...... l and rheological significance
@en
A coesite inclusion in dolomit ...... l and rheological significance
@nl
prefLabel
A coesite inclusion in dolomit ...... l and rheological significance
@en
A coesite inclusion in dolomit ...... l and rheological significance
@nl
P356
P1476
A coesite inclusion in dolomit ...... l and rheological significance
@en
P2093
Aral I. Okay
Hans-Peter Schertl
P304
P356
10.1127/EJM/6/6/0995
P577
1994-11-30T00:00:00Z