«GRAPESTONE» 관련 영어 책
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1
Microfacies of Carbonate Rocks: Analysis, Interpretation and ...
Stage 2: Increasing calcification of microbiota contributes to the formation of a
porous, cemented aggregate (grapestone) with a lobate outline. The grains are
affected by microborers leading to micritization. Stage 3: Increased cementation ...
2
Carbonate sediments and their diagenesis
of fines (10.8%) is twice that in the less turbulent oolitic and grapestone
lithofacies of the stable sand habitat. This is the reverse of what would be
expected from a comparison of turbulence. The discrepancy appears even more
remarkable if ...
Robin G. C. Bathurst, 1972
3
A Color Guide to the Petrography of Carbonate Rocks: Grains, ...
Recent sediment, north of Bimini, Bahamas These are grapestone intraclasts that
were formed on an open shelf with a low sedimentation rate. The extensively
micritized peloidal grains (mainly altered superficial ooids and skeletal fragments
) ...
Peter A. Scholle, Dana S. Ulmer-Scholle, 2003
4
Compaction of Coarse-Grained Sediments, I
A = oolitic grainstone, B = grapestone, C = angular, mixed skeletal sand, D =
valves of the pelecypod Noetia ponderosa Say, E = valves of Anomia simplex
Orbigny, and F = red algal particulate sand (data from Dunham, 1962). volume of
...
G.V. Chilingarian, K.H. Wolf, 1975
5
Carbonate Sedimentology
The grapestone belt on the Great Bahama Bank platform covers a very large area
transitional from the agitated oolite shoals to the protected pellet mud and mud
environments (Section 3.2.lc). The grapestones Binding stage 2 Grapestone ...
Maurice E. Tucker, V. Paul Wright, 2009
6
Modern Carbonate Sediments of Southern Florida, Bahamas, and ...
The younger age of sample 62-329 appears to be due to the presence of the
relatively young, al- gally-precipitated aragonite, which in combination with the
older grapestone, yields a radiocarbon age that is intermediate between that of
the ...
William Harrison Taft, John Warvelle Harbaugh, 1964
7
Modern Carbonate Environments
PLATE 1 A, Magnified view of part of grapestone grain shown in Purdy (1963, pi.
2, C). Note the similarity between the carbonate particles comprising grapestone
cement and those constituting the fecal pellet and mud aggregate illustrated by ...
Ajit Kumar Bhattacharyya, Gerald M. Friedman, 1983
8
Abstracts of papers submitted for six meetings with which ...
Sand-sized grapestone is the predominant sediment at the water—sediment
interface. Where rocks are present, they are generally covered only by one or two
inches of grapestone. The lithified zone commonly extends to 3 feet below the ...
9
Quaternary Sedimentation in South Florida
lithophagid clams) worms) Grapestone lumps" “CRYPTOCRYSTALIJNB”
Burrowing Burrow linings Scalloped rock and Lined borings (worms) GRAINS or
ENVELOPES # (Calianassa) fines (echinoids, (algae, fungi?) [Mud balls (crabs)]
...
Paul Enos, Ronald D. Perkins, 1977
10
Sedimentary Environments: Processes, Facies and Stratigraphy
... Gays oolite shoals '' i Tongue " '~ ofthe (5 E' 5 z 1 _ _ _ - - - J. “Grapestones l ' ' (
Q. _ Pellet' _ Andros l . 3 s * O mud Island (''| g - - - - (D egg/.1' " a 1'! Reel' y'
qiQoOl' (I fra mework ' lb' Coralgal ' skeletal carbonates Grapestone "_* "-7
ODlltlC ...
