「Facies」の共起表現(2語左で並び替え)

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共起表現

「Facies」の共起表現一覧(2語左で並び替え)

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of the greenschist to amphibolite metamorphic	facies and in low-temperature hydrothermal veins in a
associated with the blueschist and greenschist	facies.
alteration, often with hematite and magnetite	facies
of rocks, including granulite and amphibolite	facies, calc-silicate skarns, and quartzites; it is a
imately 90% of affected children, and peculiar	facies.
lies of the external genitalia and potter-like	facies among many others.
re diagnosable by their DNA barcodes and their	facies in Costa Rica.
t stature, developmental delay and distinctive	facies.
metamorphic grade transitional between zeolite	facies and greenschist facies representing a temperat
s important for showing a different fluviatile	facies in the top Ashdown beds from that at Brede (31
ock types belong to the Dolomitic Conglomerate	facies of the Triassic, and to the Carboniferous Lime
Smith, who used the name Hinton Sands for the	facies early in the 19th century.
inc deposits, and as a hydrothermal alteration	facies around submarine volcanism.
and epidote occur with omphacite in blueschist	facies metamorphic rocks.
rature hydrothermal phase occurring in zeolite	facies alteration of mafic rocks.
th pyrope garnet and also occurs in blueschist	facies and UHP (ultrahigh-pressure) metamorphic rocks
ame out: England's Epinomis and Jani Anglorum;	Facies Altera, which dealt with the progress of Engli
oil's components indicate a lacustrine organic	facies with lipid-rich, land-plant debris and fresh-w
up of Oligocene and early Miocene terrestrial	facies.
urana" basins with thick sequences of platform	facies rocks and /or rift related sediments.
stones and dolostones, and rocks of sanidinite	facies.
peratures and pressures typical of greenschist	facies;
Although each type of deposit (	facies) may be continuous over a wide area, its age v
uence and brackish water, in the form of tidal	facies, shark teeth, and shrimp burrows.
s a rare example of deposits of 'interstadial'	facies associated with a high sea level; these are of
sion of Pentti Eskola's concept of metamorphic	facies led to his publication of Mineralogical and St
y prehnite-pumpellyite, blueschist or eclogite	facies minerals.
idered a formation, it may be only oxbow swamp	facies within the Potomac Group.
ear mountain massifs and the radially lineated	facies of basin ejecta of the Caloris Croup surround
imalora has been identified in a wide range of	facies and locations globally.
, growth and mental retardation, progeria-like	facies, and brittle hair.
These limestones have a shallower marine	facies than contemporary sediments from the Helvetic
The prehnite-pumpellyite	facies is a metamorphic facies typical of subseafloor
etamorphic assemblages were in the amphibolite	facies, with development of metamorphic olivine-antho
The sedimentary	facies in which these fossils were found indicates th
n a metamorphosed basalt defines the Granulite	facies.
hat have been metamorphosed to the greenschist	facies.
the transition from blueschist to greenschist	facies, paragonite and glaucophane are transformed in
ocks at lower greenschist through to granulite	facies metamorphism when the rock in question is subj
The formation comprises two stratigraphic	facies, an upper thicker fine to medium sand which be
ineral in rocks metamorphosed under blueschist	facies conditions along with other sodic minerals suc
alve fauna has been found, is an unusual sandy	facies developed in the middle of the Forest Marble J

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「Facies」の共起表現一覧(2語左で並び替え)