«SERPENTINOUS»に関連する英語の本
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1
Memoirs of the Geological Survey of Great Britain, and of ...
Serpentinous Breccia. Llanfechell, Anglesey. Composed of fragments of dark
greenish serpentine cemented with veins of steatite. 74. Green Serpentine.
Llanfechell, Anglesey. With apparently a schistose structure. 75. Compact
brecciated ...
Geological Survey of Great Britain, 1865
2
A descriptive catalogue of the Rock Specimens in the museum ...
16 CAMBRIAN ROCKS, 72. Green Serpentine. Llanfechell, Anglesey. With veins
of steatite and calc spar. 73. Serpentinous Breccia. Llanfechell, Anglesey.
Composed of fragments of dark greenish serpentine cemented with veins of
steatite.
3
Chromium Geochemistry of
Serpentinous Sediment in the Willow ...
Chromium-bearing minerals such as Cr-spinel appear to be the main source of Cr in the sediment; however, Cr-bearing silicates and clay minerals are additional Cr sources. Aqueous Cr concentrations in the sediment are
United U.S. Department Of The Interior, Christopher J Oze, 2013
4
Metalliferous Mineral Deposits of the Cascade Range in Oregon
The feldspar yielded sericite, kaolin, calcite, and chloritic and serpentinous
products; the augite gave chlorite and serpentines. These alteration products
occupy the places of the original minerals. Secondary minerals, however, occur
in other ...
Eugene Callaghan, Arthur Francis Buddington, 1938
The whole seems a mass ejected from heneath, which has overflowed the
stratified rocks, appearing to cut through them on the northward, beyond the north
-west knoll, where there is a good section of the serpentinous mass resting on the
...
Henry Thomas De La Beche, 1832
The following analyses represent talcose and serpentinous rocks of varied
characters. Analyses of talcose and serpentinous rocks. A. Dark-green
serpentine, Rowe, Massachusetts. Described by B. K. Emerson in Mon. U. S.
Geol. Survey, vol.
7
Geology of the Broken Hill lode and Barrier Ranges mineral field
When examined in thin sections under the microscope, the rock is seen to consist
of a colourless isotropic groundmass and bands of vividly polarising
serpentinous fibres. The “lattice structure," so characteristic of serpentine after
hornblende, ...
8
Conservation of Building and Decorative Stone
Some marble is highly coloured; black, grey, green, pink, red, and yellow marbles
are common. Serpentine (or serpentinous) marble, also known as ophicalcite, is
a general name for marble containing a greater or lesser amount of the mineral ...
F G Dimes, J. Ashurst, 2007
9
Geology and Oil Resources of the West Border of the San ...
Big Blue serpentinous member. — The upper member of the Vaqueros, locally
known as the Big Blue, and in this report called the Big Blue serpentinous
member, is formed largely of small flakes of serpentine which make up a fine-
grained, ...
Robert van Vleck Anderson, Robert Wallace Pack, 1915
10
Talc Resources of the United States
5. Serpentinous tremolite, "10A ore," Talcville, N.Y. Typical A-2 type talc, relatively
common in Talcville region. 6. Streaked buff to chalky-tan serpentinous tremolite,
"regular ore," Talcville, N.Y. Talc somewhat transitional between A-2 and A-3 ...
Alfred Herman Chidester, Albert Edward John Engel, Lauren Albert Wright, 1964
