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Archaean and proterozoic crustal evolution in Lofoten–Vesterålen, N Norway
WL Griffin, PN Taylor, JW Hakkinen… - Journal of the …, 1978 - lyellcollection.org
The region exposes an unusually deep section through the continental crust. Gravity and
seismic surveys show a ridge-like NE-SW up-war** of the Moho to within 25 km of the …
seismic surveys show a ridge-like NE-SW up-war** of the Moho to within 25 km of the …
Buffering, infiltration, and the control of intensive variables during metamorphism
JM Rice, JM Ferry - Reviews in Mineralogy, 1982 - degruyter.com
A fundamental goal of metamorphic petrology is to understand the interrelationships and
controls of intensive variables during metamorphism. Identification of the processes that …
controls of intensive variables during metamorphism. Identification of the processes that …
Multistage metamorphic evolution and nature of the amphibolite–granulite facies transition in Lofoten–Vesterålen, Norway, revealed by U–Pb in accessory minerals
F Corfu - Chemical Geology, 2007 - Elsevier
The nature of the amphibolite-to granulite-facies transition zone exposed in the Lofoten–
Vesterålen islands of northern Norway, and the relationships between high-grade …
Vesterålen islands of northern Norway, and the relationships between high-grade …
Metasomatised xenoliths from Foster Crater, Antarctica: implications for lithospheric structure and processes beneath the Transantarctic Mountain front
Xenoliths in basanite from Foster Crater in the foothills of the Transantarctic Mountains have
been used to construct a model of the subcontinental lithosphere and lithospheric processes …
been used to construct a model of the subcontinental lithosphere and lithospheric processes …
Metamorphism of dolomites and limestones
K Bucher - Petrogenesis of metamorphic rocks, 2023 - Springer
Sedimentary carbonate rocks consist predominantly of carbonate minerals (as the name
implies). There are two main types of carbonate rocks, dolomites and limestones. The first is …
implies). There are two main types of carbonate rocks, dolomites and limestones. The first is …
Deep crustal carbonates as CO2 fluid sources: Evidence from metasomatic reaction zones
WE Glassley - Contributions to Mineralogy and Petrology, 1983 - Springer
Metasomatic reaction zones which developed at marble-pelitic schist contacts in a granulite
facies terrane in West Greenland contain a consistent sequence of five mineralogical zones …
facies terrane in West Greenland contain a consistent sequence of five mineralogical zones …
Occurrence, mineral chemistry, and metamorphism of Precambrian carbonate rocks in a portion of the Grenville Province
K RALPH, G DIANE - Journal of Petrology, 1980 - academic.oup.com
Marble occurs abundantly in a 31,000 km2 segment of the southern Grenville Province of
the Canadian Precambrian Shield, where it is associated with quartzite, biotite-garnet …
the Canadian Precambrian Shield, where it is associated with quartzite, biotite-garnet …
Crystal chemistry of Ba-rich trioctahedral micas-1M.
MF Brigatti, L Poppi - European Journal of Mineralogy, 1993 - iris.unimore.it
Ten single-crystal X-ray structure refinements of igneous and metamorphic Ba-bearing
micas were determined to define the exchange vectors required to compensate for the …
micas were determined to define the exchange vectors required to compensate for the …
Evidence for CO2 infiltration in granulite facies marbles from Lofoten-Vesteralen, Norway
AJ Baker, AE Fallick - Earth and Planetary Science Letters, 1988 - Elsevier
Lofoten-Vesteralen comprises an amphibolite to granulite facies terrain, metamorphosed in
the granulite facies at 1.8 Ga. Amphibolite facies marbles retain close to premetamorphic …
the granulite facies at 1.8 Ga. Amphibolite facies marbles retain close to premetamorphic …
Local equilibrium during the contact metamorphism of siliceous dolomites in Kasuga-mura, Gifu-ken, Japan
K Suzuki - Contributions to Mineralogy and Petrology, 1977 - Springer
The contact aureole around the Kaizuki-yama granite, recognized with a width of more than
3 km, ranges from the greenschist to the amphibolite facies. Dolomite and quartz in siliceous …
3 km, ranges from the greenschist to the amphibolite facies. Dolomite and quartz in siliceous …