「lime-stones」の共起表現(1語右で並び替え)

「lime-stones」の共起表現一覧(1語右で並び替え)

lime-stones

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Limestones and Caves of the Peak District, Geo-Books, 1
eaches are formed from a suite of mudstones, limestones and sandstones of Carboniferous age.
ly eroded valleys are cut into Mississippian limestones and below that layer Ordovician dolomites.
inely crystalline with varying sandy, clayey limestones and dolostones containing phosphate.
on environment is in serpentinized dolomitic limestones and contact metamorphosed skarns.
ment of these systems is presented mainly by limestones and dolomite.
l previous records have been from Ordovician limestones and dolomitic rocks.
Natural history includes very old Limestones and Shales laid down by the sea some 400 mil
The limestones and shales of Mortimer Forest are around 400
und in sand or clay formations, or in impure limestones and in chalk.
product of contact metamorphism of siliceous limestones and dolostones, and rocks of sanidinite faci
d Lower Carboniferous (Dinantian) Black Rock limestones and flat-bedded Upper Triassic (Rhaetian) st
The Arcadia Formation is composed of limestones and dolostones which are yellowish gray to l
The Purbeck lagoonal limestones and the shales that are exposed in the cliff
rticles of impact glass, overlain by shales, limestones and granite-derived sandstones of lower Cret
e finely crystalline, medium to thick bedded limestones and dolomites that locally contain chert sea
ally has a scattered distribution on lowland limestones and which is rare in County Durham.
on of the geology and hydrology, is given in Limestones and Caves of Northwest England, Chapter 22.
The silica-enrichment of the limestones and clays at Wurt Pit (known as the "Harptre
g marls at Devil's Punchbowl and a series of limestones and clays which have been impregnated by sil
widespread granitic intrusions; crystalline limestones and marbles; serpentinous marbles; steatite
In arid environments, limestones are often cliff-formers also.
utcrops are minor except where the overlying limestones are exposed in the north end of Fort Knox.
mudstones under the Dunham classification of limestones are also considered to be matrix-supported d
These limestones are interbedded with vuggy dolostones which
metasomatism in skarn deposits, in dolomitic limestones, associated with wollastonite, periclase, an
, and both appear to have been formed by the limestones being dissolved by subterranean waters and t
ostly siltstones and shales, with some minor limestones, between the limestones and dolomites of the
s “fist-sized” calcite inclusions within the limestones both solid and hollow with internal calcite
Siliceous limestones can be very prone to the Alkali Silica React
f shales, fine greenish tuffs, red crinoidal limestones, contorted coarse tuffs and red shales and s
Mesozoic limestones crop out north of the greywacke zone, formin
Such rocks, for example, as limestones, dolomites, quartzites and aluminous shales
ng and overturning is evident in the layered limestones exposed by quarrying at the Kentland crater.
f Mesozoic cover rocks, most notably massive limestones from the European continental shelf.
These limestones have a shallower marine facies than contempo
Carboniferous age sandstones, mudstones and limestones have generally been tilted gently to the sou
ons in the Mendips, formed by the underlying limestones having been dissolved by subterranean waters
Richterite occurs in thermally metamorphosed limestones in contact metamorphic zones.
The limestones in this interval are predominantly skeletal
The expedition examined Triassic limestones in the West Humboldt Range northeast of Reno
s a metasomatic replacement of metamorphosed limestones in the Mary Kathleen mine, Australia an in a
de deposits apparently replacing Archean age limestones in Sweden's Persberg mining district.
nd his study of fossils found in South Devon limestones informed the work of Adam Sedgwick and Roder
a late Eocene geologic formation of exposed limestones near Ocala, Marion County, Florida.
ogical time, some 230 million years ago, the limestones now exposed on Mendip formed upland areas up
ozoic turbidites (among them greywackes) and limestones of Ordovician to Devonian age; and
Paraprosopon reussi are found in the Permian limestones of the Sosio valley on Sicily (Italy).
soft shales with interbedded sandstones and limestones of late Mississippian to Pennsylvanian age.
are found in the gray Norian (late Triassic) limestones of Bad Ischl in the Austrian Salzkammergut.
Lonsdale's paper, Notes on the Age of the Limestones of South Devonshire (read 1840), was publish
derberg Plateau comprises mainly a series of limestones of early Devonian age and is one of the most
Rauna angusta, described from the Solnhofen limestones of southern Germany.
s important for study of the Inferior Oolite limestones, of Middle Jurassic age.
odusa frattigianii, known from the Solnhofen limestones of southern Germany.
nt locality for study of the Inferior Oolite limestones, of Middle Jurassic age, laid down in a warm
underlain by soft shales with sandstones and limestones of Mississippian to Pennsylvanian age.
nown as Dalton Beds, above which are Urswick Limestones, of which the limestone pavement (here and e
he Western Alps, on the formation of oolitic limestones, on kaolinization and on metalliferous veins
Purbeckian limestones, possibly from Chilmark, were used for packi
ill consists of an exposure of late Namurian limestones, sandstones and shales that form a Yoredale-
tone, the basin is filled with Carboniferous limestones, sandstones and coal measures - all of which
y below the Middle and Upper Inferior Oolite Limestones seen at Dundry Main Road South Quarry.
The site is unique in that the limestones seen here are much more closely comparable w
ea radiolarian cherts, greywacke sandstones, limestones, serpentinites, shales, and high-pressure me
Other important rock formations include limestones, shales, and conglomerates.
as tetragonal crystals in skarn deposits and limestones that have been subjected to contact metamorp
cally associated with copper deposits around limestones, the source of the carbonate.
cal Composition of the Silurian and Cambrian Limestones; The Geology of Bolivia and Southern Peru an
roperties of sedimentary rocks, particularly limestones, their formation and usefulness as an oil re
When found in Palaeozoic limestones, they typically indicate depositional depth
nce of Carboniferous Limestone, and includes limestones, thick volcanic tufts and lavas are exposed,
The section exposed runs from the Blues Limestones through the Plant and Bone Beds, the Cinder
Limestones were deposited upon peripheral bulges in the
Devonian limestones were found in Telen River, East Kalimantan,
The succession is composed of Givetian limestones, which are separated by a thrust from a Fras
He worked exclusively with limestones which were delivered to him by the wrecking
In the past it has been debated whether the limestones, which are of Middle Cambrian age (ca.
layer cake of Palaeozoic era sandstones and limestones which dip gently southwards into the South W
The limestones which make up the mountains are white to pal
o notable is the fact that the Jamesoni Zone limestones which occur here are much thicker and better
lack Down and Downhead and the Carboniferous Limestones, which dominate the hills and surround the o
d of Pulpit Rock), then a cap of thin-bedded limestones which are part of the basal Purbeck Formatio
ts shallow northern scarp, are Carboniferous Limestones whilst above these is the coarse Twrch Sands
In the eastern section there are Jurassic limestones with halite (rock salt) deposits.
ll of these rocks are generally thick bedded limestones with chert, gypsum, dolomite.