「ejecta」の共起表現(1語右で並び替え)

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共起表現

「ejecta」の共起表現一覧(1語右で並び替え)

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the crater; lobate flows emanating from crater	ejecta, and very radar-bright ejecta and floor.
cts excavated and mixed dark material into the	ejecta and the resulting mix is not apparent against
ast of the crater rim, emplacement of hummocky	ejecta appears to have been impeded by the topography
The	ejecta are mainly observed to the north and northeast
hock effects are tectonic features, the impact	ejecta are Quaternary alluvial fans or Tertiary congl
This alder	ejecta area is on spectrographic evidence instead pri
The dark annulus of	ejecta around Tolstoj is one of the darkest places on
The plains may be impact deposits (	ejecta) associated with Ursula or they may be cryovol
	Ejecta blanket from Hadley crater filling in Hadley R
The	ejecta blanket becomes thinner with distance and incr
Valleys on the	Ejecta Blanket from Cerulli Crater, as seen by HiRISE
The result is that both the crater and its	ejecta blanket stand above the surroundings.
r an impact event, the falling debris forms an	ejecta blanket surrounding the crater.
Its extensive	ejecta blanket and secondary crater field are superpo
An	ejecta blanket is a generally symmetrical apron of ej
ter has an inner and an outer ring and a small	ejecta blanket surrounding the outer ring.
It is on the edge of the much larger	ejecta blanket surrounding the crater Victoria, named
It is a dark-floored crater with a bright	ejecta blanket located in the Uruk Sulcus region.
Asymmetries in the crater structure and the	ejecta blanket imply that the projectile impacted at
Emma Dean lies directly on top of the	ejecta blanket from Victoria and could therefore expo
he northwestern section of Abedin's continuous	ejecta blanket appears to have a lower reflectance th
s (15 mi) in diameter, and is surrounded by an	ejecta blanket of breccia preserved over an area of 6
ly sloped scarp that terminates the continuous	ejecta blanket.
Similar features may be seen in	ejecta blankets of Martian craters, suggesting impact
gists associate the glass not with impact melt	ejecta, but with radiative melting from meteoric larg
s estimated that immediately after the impact,	ejecta covered an area of 25,000 square kilometres (9
The presence of hummocky, radar-bright crater	ejecta crossing the radar-dark floor terrace and adja
It has an outer lobate	ejecta deposit extending about a crater radius from t
The	ejecta deposit surrounding the craters appears very b
simultaneously, it is difficult to discern any	ejecta deposit on the dark terrain.
nded by a system of bright rays, which are ice	ejecta deposited during the impact event.
low, hummocky rim material that may consist of	ejecta deposits.
nding site area is believed to be blanketed by	ejecta excavated by the impact that created Heimdal.
Approximately half the volume of	ejecta falls within 1 crater radius of the rim, or 2
Centered on the impact crater, a wide	ejecta field has been traced, some 50 km across, form
ge of the outer ramparts of Langrenus, and the	ejecta forms low ridges attached to the south rim of
s have suggested that angrites could represent	ejecta from Mercury.
ounding Abedin are secondary craters formed by	ejecta from the initial impact.
crater floor is faintly marked by lighter-hued	ejecta from the crater Giordano Bruno to the north.
he crater floor has been resurfaced, either by	ejecta from the Mare Imbrium or by basaltic lava, and
lanitia is part of (Caloris Planitia) might be	ejecta from Caloris that were melted by the impact.
rt of the rim of Bingham is partly overlaid by	ejecta from Lobachevsky.
ed by the mare and overlain across the east by	ejecta from Alpetragius.
In particular, if the	ejecta from a crater formed in the highlands (which i
face, its features eroded and blanketed by the	ejecta from the relatively fresh crater Antoniadi jus
believed that both Esclangona and its moon are	ejecta from an asteroidal collision in the past that
ater is geologically young as the fresh impact	ejecta has rough surface, which is a good scatterer o
hile the pristine state of preservation of the	ejecta has been used to suggest that it may in fact b
The "skirt" of	ejecta in this case is due to a tangential release of
ides of the wave, gravitationally grouping the	ejecta into a plane.
n Yuty's southwestern rim is evidence that the	ejecta is thin.
s typical volcanoes do; instead, a low ring of	ejecta known as a tuff ring forms around a bowl-shape
Nature of dominant	ejecta: lithic, blocks and ash; often accretionary la
les) in diameter, and is surrounded by complex	ejecta lobes, which are a distinctive characteristic
raters, the amount, distribution, and sizes of	ejecta, mechanical properties of the surface such as
al and mid-latitudes on Mars have this form of	ejecta morphology, which is thought to arise when the
Its type occurrence is within the limestone	ejecta of the Mount Vesuvius volcano complex near Nap
sifs and the radially lineated facies of basin	ejecta of the Caloris Croup surround the Caloris Basi
Some fiamme represent fragments of volcanic	ejecta, often pumice lapilli that have been flattened
, steep-sided, and often display no associated	ejecta or lava flows.
nteraction of crater materials (the meteoroid,	ejecta, or both) and high-speed winds in the upper at
ed by secondary impacts of the larger crater's	ejecta or by volcanic venting activity along a rift.
in near the crater and associated with impact	ejecta or hot water precipitates form crater ridges a
ummocky remnants resembling basin deposits and	ejecta protrude above the gently sloping basin wall.
A pedestal crater is a crater with its	ejecta sitting above the surrounding terrain.
The outer rampart of	ejecta spills over slightly into the Apollo basin flo
ndary craters are impact craters formed by the	ejecta that was thrown out of a larger crater.
the larger crater Lewis, in the outer skirt of	ejecta that surrounds the Mare Orientale impact basin
rochronology, Saksunarvatn tephra are volcanic	ejecta that form an ash layer that is useful in datin
A ray system comprises radial streaks of fine	ejecta thrown out during the formation of an impact c
	Ejecta which falls within that area is considered pro
volcanic material (both solidified magma, and	ejecta) which appears mostly flat from the surface.

共起表現

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「ejecta」の共起表現一覧(1語右で並び替え)