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「facies」の共起表現一覧(2語右で並び替え)

該当件数 : 34



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


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