「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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