「CARBONIFEROUS」の共起表現(1語右で並び替え)

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共起表現

「CARBONIFEROUS」の共起表現一覧(1語右で並び替え)

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e cut into mudstones and sandstones of the	Carboniferous age Coal Measures.
The overlying Devonian and	Carboniferous age sandstones, mudstones and limestones h
There is an area of sandstone and shale of	Carboniferous age in the north east, and the Lizard peni
The hill is formed from a succession of	Carboniferous age sandstones and mudstones, notably the
zone of coarse-grained biotite granite of	Carboniferous age, intruded into surrounding Devonian ag
ntaining shales of Upper Devonian to Lower	Carboniferous age, has been extensively studied during t
is formed from a series of rock strata of	Carboniferous age, each of which dip moderately southwar
Paleozoic sedimentary rocks of Permian and	Carboniferous age, that lie unconformably upon Precambri
of mudstones, limestones and sandstones of	Carboniferous age.
rmerly included in Halicyne of mid to late	Carboniferous age.
rmed from the more readily eroded rocks of	Carboniferous age.
-lying succession of sedimentary strata of	Carboniferous age.
tion, (Langsettian or Westphalian A, Upper	Carboniferous); also Indiana, Kansas (USA), and Spain, (
basis for a geological period between the	Carboniferous and the Silurian: the Devonian Period.
e period including the latter parts of the	Carboniferous and early part of the Permian period.
al activity spanned virtually the whole of	Carboniferous and Early Permian time (A.G.
volcanic rock and sedimentary rocks of the	Carboniferous and Permian periods.
rifted north from Gondwana during the Late	Carboniferous and collided against eastern Laurasia (the
ocks to the west and separates the younger	Carboniferous and Permo-Triassic rocks of the Vale of Cl
ry reptile-like amphibians dating from the	Carboniferous and Permian periods, or to amniotes and th
as distinguished for his researches on the	Carboniferous and Cretaceous rocks and fossils of Saxony
Toward the end of the	Carboniferous, around 290 million years ago, Gondwana, t
but the fault zone was reactivated in the	Carboniferous as a NW-throwing normal fault with seismic
Flora of the outlying	Carboniferous basins of southwestern Missouri US Geologi
ot evenly spread over the county, with the	Carboniferous beds being only found in the far north of
stone of the Avon Group and younger marine	Carboniferous Black Rock Limestone.
Indeed, some 56 species of early	Carboniferous brachiopods alone were discovered in this
Keele Clay - a	Carboniferous clay
, a hard sandstone marking the base of the	Carboniferous Coal Measures.
re the underlying geology is predominantly	Carboniferous coal measures.
one Grit outcrop onto the mudstones of the	Carboniferous Coal Measures.
the Pottsville Form, (Westphalian A, Upper	Carboniferous, coal mine and tailings); also Indiana, Ka
By the	Carboniferous, coleoids already had a diversity of forms
Joanellia is an extinct genus of	Carboniferous crustacean.
his contributions on the field of Permo -	Carboniferous ecosystems.
n sedimentary rocks laid down in the Early	Carboniferous era some 360 to 320 million years ago.
term relating to strata at the base of the	Carboniferous formation, below the entire sequence of co
extinct genus of harvestmen known from the	Carboniferous fossil record.
las strata is spread over the Devonian and	Carboniferous geological periods.
dramatic cliffs and overlooks eroded from	Carboniferous gray sandstone.
Araeoscelida are known from the Late	Carboniferous in the United States (Petrolacosaurus, Spi
mericlus contains several species from the	Carboniferous, including A. americanus (formerly Cyclus
has yielded the largest ever collection of	Carboniferous insects in Britain.
arus is one of the most abundant genera of	Carboniferous insects.
Until the three collided in the	Carboniferous, it created the Ural Mountains, completely
d Red Sandstone rocks to the north and the	Carboniferous Limestone rocks to the south.
valleys cut through the rim of the basin,	carboniferous limestone and sandstone is exposed, allowi
s are still at work in the area, providing	Carboniferous limestone for road surfacing and also Penn
, vol lxii); 'The Faunal Succession in the	Carboniferous Limestone of Westmorland' (Geol Mag, 1907)
	Carboniferous limestone
The chapel is constructed in rubble	carboniferous limestone with ashlar gritstone dressings.
The underlying rocks are almost entirely	carboniferous limestone with a small amount of Triassic
consists of an underground waterway in the	Carboniferous Limestone of South Wales.
The ground floor is of	carboniferous limestone and the upper floors are brick w
	Carboniferous limestone fossil record of the Peak Distri
It lies on	carboniferous limestone with rock showing through the th
The summit is formed from	Carboniferous Limestone whilst much of the Cefn Cadlan r
Broken cliffs of	Carboniferous Limestone occur along the northern edges a
The island is formed of	carboniferous limestone and is geologically a continuati
ral underground cave systems formed in the	Carboniferous Limestone many millions of years ago.
omerate facies of the Triassic, and to the	Carboniferous Limestone series.
One of the stones of	carboniferous limestone had been sculpted into a shape r
15571) is a cave near Charterhouse, in the	carboniferous limestone of the Mendip Hills, in Somerset
5) is a cave near Stoke St Michael, in the	carboniferous limestone of the Mendip Hills, in the Engl
motte and bailey castle built in a natural	carboniferous limestone outcrop, grid reference SD742416
ngdown is at the end of a dry valley where	Carboniferous Limestone outcrops as a small cliff, oppos
western edge of the Lulsgate Plateau, the	Carboniferous limestone hills which form a northern outl
ck Rock, Vallis and Clifton Down Groups of	Carboniferous Limestone with overlying buff-coloured Jur
s Blaen-nedd-isaf where they encounter the	Carboniferous Limestone outcrop.
north east of the camp actively extracted	carboniferous limestone in the 20th century and demonstr
The immediately underlying	Carboniferous Limestone has dissolved away in numerous l
o its north are large quarries working the	Carboniferous Limestone outcrop which parallels the narr
k Dolomite and Black Rock Limestone of the	Carboniferous Limestone Series.
It enters onto the	Carboniferous Limestone outcrop near this point and sect
ern and western flanks is a narrow band of	Carboniferous Limestone which gives rise to a karst land
stage/age (which corresponds to the upper	Carboniferous Limestone of Great Britain) and succeeded
The quarry exhibits pale to dark grey	Carboniferous Limestone with small area of overlying hor
debris scree which had formed against the	Carboniferous limestone cliffs of the gorge.
e which occur in major fissures within the	Carboniferous Limestone laid down beneath the sea some 3
by the uplift, folding and faulting of the	Carboniferous Limestone, periodically opened and closed
nderlying rocks are Devonian sandstone and	Carboniferous limestone, overlain by with Triassic Dolom
of approximately 0.25M tonnes per year of	Carboniferous Limestone, for general purpose constructio
of slate, and the valley sides are made of	carboniferous limestone, and both sides have scars on th
Made of	carboniferous limestone, it is a continuation of the Men
It is	Carboniferous limestone, at its highest point it is 58 m
pment is formed from two distinct bands of	Carboniferous limestone, the Glencar Limestone Formation
uarry which is operated by Tarmac produces	Carboniferous Limestone, which is mainly for use on the
The lower section is made up of	Carboniferous Limestone, a softer rock which is more eas
The woodland sits on a ridge of	Carboniferous limestone, and its slopes are covered with
rry exhibits pale to dark grey well-bedded	Carboniferous Limestone, about 350-320 million years old
At Middle Hope a sequence of	Carboniferous Limestone, and includes limestones, thick
It is a dark, fine-grained, muddy	Carboniferous limestone, rich in bitumen which gives it
h are surrounded by the younger flat-lying	Carboniferous Limestone.
hern slopes are formed from the underlying	Carboniferous Limestone.
ws red Triassic rocks in fissures of older	carboniferous limestone.
adjoining fells are mainly a bed of hard,	carboniferous limestone.
exposures are cut in very steeply-dipping	Carboniferous Limestone.
rry exhibits pale to dark grey well-bedded	Carboniferous Limestone.
located in a comparatively narrow band of	carboniferous limestone.
and the Twrch Sandstone which overlie the	Carboniferous Limestone.
abundant marine borings in the top of the	Carboniferous Limestone.
consists of a steep-sided ravine cut into	Carboniferous Limestone.
mitic Conglomerate unconformably overlying	Carboniferous Limestone."
osed along its shallow northern scarp, are	Carboniferous Limestones whilst above these is the coars
ble around Black Down and Downhead and the	Carboniferous Limestones, which dominate the hills and s
ld Red Sandstone, the basin is filled with	Carboniferous limestones, sandstones and coal measures -
Ordovician, Silurian, Devonian, and early	Carboniferous, marine sedimentation left extensive depos
Lower	Carboniferous, Montana, USA
n particular it is the various beds of the	Carboniferous Namurian age 'Minn Sandstone' which have w
Upper	Carboniferous of northeastern Ohio.
tinct genus of temnospondyl from the Upper	Carboniferous of the Czech Republic.
n extinct genus of scorpion from the Upper	Carboniferous of Europe and North America.
Fossil seed fern leaves from the Late	Carboniferous of northeastern Ohio.
r genus to the varanopid family from Upper	Carboniferous of United States.
Turner, 1954, has been found in the Lower	Carboniferous of Ireland and the Isle of Man.
extinct genus of shark which lived in the	Carboniferous of North America and Russia.
f carnivorous stem tetrapod from the Early	Carboniferous of Scotland and possibly Greer, West Virgi
iatitina, that lived during the very early	Carboniferous of what is now Russia.
s the sandy beds near the end of the lower	Carboniferous of the west of England, for example the Dr
timated to be less than 345 million years (	Carboniferous or younger).
aleobiologist and carried out some work on	carboniferous palaeobotany.
escribed as "one of the founders of modern	Carboniferous palynology".
ich is believed to have existed during the	Carboniferous period when what is now the Peak District
mountain building episode (orogeny) in the	Carboniferous Period of geological history.
f Northumberland were laid down during the	Carboniferous Period when variations in sea level result
Its coal seams were laid down in the	Carboniferous period and some easily accessible seams we
During the prehistoric	Carboniferous period it was a sea floor and later a trop
Eophrynids lived during the	Carboniferous period in what is now modern Europe and No
Mycterops lived in the	Carboniferous period in Europe and North America.
metres thick, and was laid down during the	Carboniferous period some 350 million years ago.
extinct genus of tetrapods from the Early	Carboniferous period (late Visean) of North America.
ia (Labyrinthodont) that lived in the Late	Carboniferous period (Moscovian) (300 million years ago)
ct genus of lepospondyl amphibian from the	Carboniferous period of Europe and North America.
of early ray-finned fish that lived in the	Carboniferous period of Europe.
otarbid group, which lived during the Late	Carboniferous period in Europe.
nt lobe-finned fish which lived during the	Carboniferous period in Australia.
prehistoric reptiles which appeared in the	Carboniferous period and became extinct after the Early
s steep limestone cliffs, laid down in the	Carboniferous period some 350 million years ago.
During the	Carboniferous period (circa 300 million years before the
s of fossil seed ferns that existed in the	Carboniferous period (around 360 to 300 million years ag
, lobe-finned fish, which lived during the	Carboniferous period (Serpukhovian stage, about 318 - 32
e limestone that usually originated in the	Carboniferous period but a less pure limestone from the
ic lobe-finned fish which lived during the	Carboniferous period (Early Pennsylvanian to Late Missis
Ilkley Moor, in the	Carboniferous period 325 million years ago, was in a swa
of Falcatidae which lived during the early	Carboniferous Period in Bear Gulch bay and what is now M
stones ('gritstones') also dating from the	Carboniferous period and which have foundered in many pl
n from the Mississippian sub-period of the	Carboniferous Period, about 330 million years ago.
hich lived from the Ordovician to the Late	Carboniferous period, were characterized by small to lar
of the Hercynian mountain building of the	Carboniferous period, about 350 to 250 million years ago
During the	Carboniferous period, fungi and bacteria had yet to evol
ch were laid down in a delta system in the	Carboniferous period.
rit Series) which was laid down during the	Carboniferous period.
laid down during the Namurian stage of the	Carboniferous period.
They appeared in the late	Carboniferous period.
Pterygochiton became extinct during the	Carboniferous period.
Glyptochiton became extinct during the	Carboniferous period.
is extinct family of sharks existed in the	Carboniferous period.
hillips and William Conybeare identify the	Carboniferous Period.
It inhabited the large swamps of the	Carboniferous Period.
rehistoric lungfish which lived during the	Carboniferous period.
genus of labyrinthodont that lived in the	Carboniferous period.
ic lobe-finned fish which lived during the	Carboniferous period.
f sandstones and mudstones dating from the	Carboniferous Period.
ont lobe-finned fish that lived during the	Carboniferous period.
ae is an extinct family of sharks from the	Carboniferous period.
y of amphibian tetrapods that lived in the	Carboniferous period.
a layer cake of rocks laid down during the	Carboniferous period.
s of temnospondyl amphibian from the Early	Carboniferous period.
ostracod crustacean that lived during the	Carboniferous period.
tinct genus of Onychophoran known from the	Carboniferous period.
inant part of the world's flora during the	Carboniferous period.
fishes which lived during the Devonian and	Carboniferous period.
ich lived from the Ordovician to the Upper	Carboniferous period.
apods that lived in the rivers of the Late	Carboniferous period.
lived from the Late Silurian to the Early	Carboniferous period.
laid down during the Namurian stage of the	Carboniferous period.
mya in the mid-Pennsylvanian Epoch of the	Carboniferous Period.
sbian sub-stage of the Visean stage of the	Carboniferous period.
Basin Province which originated during the	Carboniferous period.
0-350 million years ago in the Permian and	Carboniferous periods.
Numerous Devonian and	Carboniferous plutons are also found.
ning occurred for a time in the underlying	Carboniferous rock strata and the subsidence of these wo
	Carboniferous rocks give rise to the Bristol coalfield i
- 'On some New Crustaceans from the Lower	Carboniferous Rocks of Eskale and Liddesdale' (Trans Roy
ult which throws the relatively flat-lying	Carboniferous rocks of the area down to the south.
Its base is an unconformity on top of	Carboniferous rocks of the Limburg Group, which are more
hich represents the best exposure of Upper	Carboniferous rocks in the Avonmouth Coalfield.
he only part of Cornwall that is formed of	carboniferous rocks, the northern area of North Cornwall
ype of branching tree root fossil found in	Carboniferous rocks.
een these two layers is a thinner layer of	Carboniferous sandstone, which was baked hard when the W
family, Koninckioceratidae, found in Lower	Carboniferous sediments in Europe, and named by Hyatt, 1
omycetes) infecting the stem cortex of the	Carboniferous seed fern Lyginopteris oldhamia".
	~Carboniferous, Siberia collided with the minor continent
Anthracosaurus from the Late	Carboniferous some 310 million years ago, was a large, a
t coalfield, including 3,000 tons of Upper	Carboniferous spoil from which more than 1,400 insect fo
terest, which includes 3,000 tons of Upper	Carboniferous spoil from which more than 1,400 insect fo
iplovertebron punctatum inhabited European	Carboniferous swamps (nowadays Czech Republic), where it
ian age - a subdivision of the NW European	Carboniferous system from ca 315 to 326.4 Ma, which occu
It is a subdivision of the	Carboniferous system or period and the regional Silesian
erm for the coal-bearing part of the Upper	Carboniferous System.

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共起表現

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

「CARBONIFEROUS」の共起表現一覧(1語右で並び替え)