-
elements within the
Earth according to
their preferred host
phases into
lithophile (rock-loving),
siderophile (iron-loving),
chalcophile (sulfide ore-loving...
-
Lithophiles are micro-organisms that can live
within the pore
interstices of
sedimentary and even
fractured igneous rocks to
depths of
several kilometers...
- magnitude.
Colour indicates each element's
Goldschmidt classification:
Lithophile Siderophile Atmophile Chalcophile Trace
Abundances of the elements...
-
Metallic elements are
primarily found as
lithophiles (rock-loving) or
chalcophiles (ore-loving).
Lithophile elements are
mainly the s-block elements,...
- rubidium, caesium, strontium, and
barium (called LILE, or large-ion
lithophile elements), and the
other group includes elements of
large ionic valences...
- evolution. This
enrichment in REEs,
along with a
moderate to high large-ion
lithophile element (LILE)
enrichment (ΣLILE > 1,000 ppm)[clarify],
including elements...
-
chondrites are
distinguished chemically by
their depletions in
refractory lithophile elements, such as Ca, Al, Ti, and rare earths,
relative to Si, and isotopically...
- mantle,
resulting in two
types of
mantle reservoirs:
those depleted in
lithophile elements (depleted reservoirs), and
those composed of "fresh" undifferentiated...
- processes.
Heavy metals are
found primarily as
lithophiles (rock-loving) or
chalcophiles (ore-loving).
Lithophile heavy metals are
mainly f-block
elements and...
- reactivity, do not
occur naturally in pure form in nature. They are
lithophiles and
therefore remain close to the Earth's
surface because they combine...
