「Facies」の共起表現一覧(1語右で並び替え)
該当件数 : 35件
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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