「Mudstone」の共起表現(1語右で並び替え) - Weblio英語共起表現検索


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Weblio 辞書 > 英和辞典・和英辞典 > Mudstoneの意味・解説 > Mudstoneに関連した共起表現

「Mudstone」の共起表現一覧(1語右で並び替え)

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ands of coarse sandstone (or 'gritstone') and mudstone all of which are assigned to the Namurian age
ng 5 m are light-yellowish-gray to olive-gray mudstone and shale.
This is composed of laminated mudstone and siltstone with greywacke sandstone and is
andstones with small amounts of finely-bedded mudstone and mudstone arranged in rhythmic units ("cyc
mposed mainly of Ordovician and some Silurian mudstone and limestone.
ntative of the Kirkstile Formation, laminated mudstone and siltstone also typical of the Skiddaw gro
Barrow is composed of the laminated mudstone and siltstone of the Kirkstile Formation, typ
Formation (fossiliferous shale and calcareous mudstone), and is near the axis of a syncline in the c
nd sedimentary rocks, including sandstone and mudstone, and lies unconformably on top of older Devon
Expansion and contraction of the supporting mudstone around the inflexible clasts actually left se
There is Dolomitic Conglomerate (Triassic Mudstone) at the lower edges of the site.
composed of alternate layers of sandstone and mudstone dating from the Devonian period and ascribed
omorph from upper Permian (upper Roadian age) mudstone deposits of Dashankou locality, Xidagou Forma
omorph from upper Permian (upper Roadian age) mudstone deposits of Dashankou locality, Xidagou Forma
ue to the softer adjacent strata of shale and mudstone eroding at a faster rate than the hard wearin
Mudstone formation on Lyme Regis East Beach.
d in turn by the thick sequence of the Raglan Mudstone Formation.
the softer mudstones of the underlying Raglan Mudstone Formation.
e Tarporley Siltstone Formation of the Mercia Mudstone Group.
Zircons in the sandstone and underlying mudstone indicate an age of 104.46 ± 0.95 million year
it Lake Formation has a lower member of black mudstone inserted with beds of iron formation and unit
Above the red mudstone is green mudstone, folllowed by the Rhaetic b
Here the clay bedrock plateau (Mercia Mudstone) is dissected by a number of streams, forming
lie between layers of softer marine clays and mudstone, laid down in repeated marine ingressions, mi
Siltstone and mudstone layers can be calcareous and feature dolomiti
in a calcareous nodule recovered from a silty mudstone matrix.
otal, contains two subdivisions, the Svarvare Mudstone Member, two to three metres thick, which is o
ormation which show through the limestone and mudstone of the Avon Group and younger marine Carbonif
e deposited by streams and contain limestone, mudstone, quartzite and volcanic cobbles that are up t
edimentary and alluvial deposit: marl, Mercia mudstone, sand and gravel ("Burtle Beds"), peat, and d
The Paskapoo Formation is composed of mudstone, siltstone and sandstone, with subordinate li
olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone.
olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone.
From the east to west there are, mudstone, State Circle Shale, and then micaceous Black
The orange clay is the Mercia Mudstone that underlies this area of Birmingham and wo
fossil bearing and variably sandy and clayey mudstone, wackestone, and packstone with little to no
Until the 1990s, mudstone was exhausted in the mine of the brickyard in
The section is primarily mudstone, which yields an abundance of shelly faunas.
The whole area is underlain by Silurian mudstone which was extensively glaciated during the la
ne is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and
All the stones are mudstone, which, as with those used at Tinkinswood, we
The subsoil is Keuper Marl (Mercia Mudstone) with a band of Keuper Sandstone (Bromsgrove
s good sections of Upper Kimmeridge shale and mudstone, with some bituminous shale and some small ca
The lower part of the cliff is a red mudstone, with bands of nodules of pinkish-white alaba
                                                                                                    


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