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「Facies」の共起表現一覧(1語右で並び替え)

該当件数 : 35



ame out: England's Epinomis and Jani Anglorum; Facies Altera, which dealt with the progress of Engli
rature hydrothermal phase occurring in zeolite facies alteration of mafic rocks.
lies of the external genitalia and potter-like facies among many others.
The formation comprises two stratigraphic facies, an upper thicker fine to medium sand which be
tone Member here is calcareous (Tilgate Stone) facies and probably only the proximal (pro-fan-delta)
imalora has been identified in a wide range of facies and locations globally.
metamorphic grade transitional between zeolite facies and greenschist facies representing a temperat
of the greenschist to amphibolite metamorphic facies and in low-temperature hydrothermal veins in a
, growth and mental retardation, progeria-like facies, and brittle hair.
th pyrope garnet and also occurs in blueschist facies and UHP (ultrahigh-pressure) metamorphic rocks
inc deposits, and as a hydrothermal alteration facies around submarine volcanism.
s a rare example of deposits of 'interstadial' facies associated with a high sea level; these are of
of rocks, including granulite and amphibolite facies, calc-silicate skarns, and quartzites; it is a
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
Smith, who used the name Hinton Sands for the facies early in the 19th century.
The sedimentary facies in which these fossils were found indicates th
s important for showing a different fluviatile facies in the top Ashdown beds from that at Brede (31
re diagnosable by their DNA barcodes and their facies in Costa Rica.
The prehnite-pumpellyite facies is a metamorphic facies typical of subseafloor
sion of Pentti Eskola's concept of metamorphic facies led to his publication of Mineralogical and St
Although each type of deposit ( facies) may be continuous over a wide area, its age v
and epidote occur with omphacite in blueschist facies metamorphic rocks.
ocks at lower greenschist through to granulite facies metamorphism when the rock in question is subj
y prehnite-pumpellyite, blueschist or eclogite facies minerals.
ock types belong to the Dolomitic Conglomerate facies of the Triassic, and to the Carboniferous Lime
ear mountain massifs and the radially lineated facies of basin ejecta of the Caloris Croup surround
the transition from blueschist to greenschist facies, paragonite and glaucophane are transformed in
urana" basins with thick sequences of platform facies rocks and /or rift related sediments.
Two facies series are the Franciscan and Sanbagawa types.
uence and brackish water, in the form of tidal facies, shark teeth, and shrimp burrows.
These limestones have a shallower marine facies than contemporary sediments from the Helvetic
etamorphic assemblages were in the amphibolite facies, with development of metamorphic olivine-antho
oil's components indicate a lacustrine organic facies with lipid-rich, land-plant debris and fresh-w
idered a formation, it may be only oxbow swamp facies within the Potomac Group.
                                                                                                    


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