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Magma
Magma Mag"ma, n. [L., fr. Gr. ?, fr. ? to squeeze, knead.]
1. Any crude mixture of mineral or organic matters in the
state of a thin paste. --Ure.
2. (Med.)
(a) A thick residuum obtained from certain substances
after the fluid parts are expressed from them; the
grounds which remain after treating a substance with
any menstruum, as water or alcohol.
(b) A salve or confection of thick consistency.
--Dunglison.
Meaning of Magmas from wikipedia
-
silicic magmas have a
silica content greater than 63%. They
include rhyolite and
dacite magmas. With such a high
silica content,
these magmas are extremely...
- is a
function from X to any
magma N, then
there is a
unique extension of f to a
morphism of
magmas f′ f′ : MX → N.
Magmas are not
often studied as such;...
- of
magmas, with
magmas as
objects and
morphisms given by
homomorphisms of
operations Magma (band), a
French experimental progressive rock band
Magma (Magma...
-
Magma Aviation is a
European cargo handler specialising in
charter and
regular cargo services.
Magma Aviation runs
regular B747-400F
services between cargo...
-
Magma is the self-titled
debut album by
French rock band
Magma.
Released as a double-LP in 1970, it is a
concept album which tells the
story of a group...
- In mathematics,
there exist magmas that are
commutative but not ****ociative. A
simple example of such a
magma may be
derived from the children's game...
- A
magma chamber is a
large pool of
liquid rock
beneath the
surface of the Earth. The
molten rock, or
magma, in such a
chamber is less
dense than the surrounding...
- calc-alkaline
magma series by the
redox state of the
magma they
crystallized from (tholeiitic
magmas are reduced; calc-alkaline
magmas are
oxidized )...
-
Hydrous magmas composed of
basalt and
andesite are
produced directly and
indirectly as
results of
dehydration during the
subduction process. Such
magmas, and...
- from the rare
peralkaline magmas,
which have
excess alkali oxides relative to
alumina (Na2O + K2O > Al2O3).: Ch6
Alkaline magmas tend to show high titanium...
