On-Line Catalog Page 3
Conditions of Sale Mineralogy samples from the Earth's mantle are some of the rarest and most difficult geologic materials for educators, collectors and the scientific community to acquire. The samples listed are offered on a first-come, first serve basis and guaranteed to be exactly as described. All major credit cards accepted including PayPal. Checks are welcome but please email us first so that we may confirm availability and hold the material until your check arrives. |
Questions on any specimens? lab@petrologyslides.com |
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Spinel harzburgite, Lambert-Amery Rift system, in thin section |
Spinel harzburgite, Lambert-Amery Rift system, groundmass |
Spinel harzburgite, Lambert-Amery Rift system, Jetty Penninsula, East Antarctica | Spinel harzburgite, Lambert-Amery Rift system, polished slice |
From the Severnoe Verkhnee
multi-phase intrusive body. A fresh rock delivered from the upper mantle by the
host magma. Mineralogy: olivine, orthopyroxene and subordinated chrome-spinel.
Harzburgites are rarely seen in the East Antarctic volcanic rocks. Collected
during the Australian summer of 1986 near the western edge of the Lambert
Glacier, East Antarctica. |
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Specimen# 41-100 | |
Perovskite Magnetite Dunite in thin section |
Perovskite Magnetite Dunite |
Perovskite Magnetite Dunite, Mata da Corda Formation, Minas Gerais, Brazil | |
Presidente Oligario volcanics,
Mata da Corda Formation, Minas Gerais, Brazil. Fresh olivine is scarce in these
volcanics which generally are lamproite-ugandite composition but the olivine in
this specimen of perovskite-magnetite dunite is quite fresh. This is an
extremely dense rock. |
|
Specimen# 42-99 | |
Eclogite, Borborema Province, Pernambucco, in thin section |
Eclogite, Borborema Province, Pernambucco matrix |
Eclogite, Borborema Province, Pernambucco, Brazil | Eclogite, Borborema Province, Pernambucco matrix |
Eclogites are some of the most
dramatic appearing rocks to be transported from the upper mantle. The Borborema
Province, in the NE of Brazil, is a rather complex piece in the Brazil-Africa
puzzle and a world-class locality of extraordinary geologic diversity.
Eclogites consist primarily of green pyroxene (omphacite) and red garnet
(pyrope), with small amounts of various other stable minerals i.e., rutile.
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Specimen# 43-90 | |
Olivine Melilite in thin section |
Olivine Melilite groundmass |
Olivine Melilite Hypabyssal Rock, Jusiberg diatreme, Urach volcanic field, Rhine Graben, Germany | Olivine Melilite slice |
This is a very fresh, rare,
intrusive rock with glassy phenocrysts of olivine. Samples also contain
phenocrysts of melilite, and clinopyroxene with groundmass perovskite and thin
zeolitic veins. Research indicates that these melilitites are near-primary
magmas, probably derived as small-degree partial melts from the base of the
lithosphere, which had previously been enriched over time by melts ascending
from the asthenosphere below. Melt production in the asthenosphere is believed
to have begun at 100-200 km depth beneath the Rhinegraben, within the
dolomite-phlogopite-garnet stability field. |
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Specimen# 44-98 | |
Thin section unavailable. |
Dunite with Wehrlite veins. |
Dunite with Wehrlite veins, Lewis Hills Massif, Bay of Islands Ophiolite, Newfoundland | Dunite with Wehrlite veins. |
This is coarse dunite
(peridotite) with even coarser clinopyroxenite (wehrlite) veins. It's a
completely undeformed intrusive rock emplaced within upper mantle residual
harzburgite. In summary, a coarse dunite (peridotite) was intruded by multiple
generations of wehrlite (clinopyroxenite). In the polished surface there are
visible small black grains of chromite. |
|
Specimen# 45-97 | |
Benmoreite in thin section |
Benmoreite surface |
Benmoreite, transistional between Alkali Basalt and Trachyte. Lenderut Hills, Rift Valley, Kenya | Benmoreite prepared section |
Benmoreites are extrusive,
transistional, members of the alkali basalt magma series. With increasing
magmatic differentiation, by inceasing SiO2 content, the series is alkali
basalt-hawaiite-mugearite-benmoreite-trachyte. The type locality after which
the rock is named is Ben More on the Isle of Mull, Scotland. |
|
Specimen# 46-86 | |
Kenyte thin section not available |
Kenyte (anorthoclase phonolite) |
Kenyte (anorthoclase phonolite), Meteorological Station, Mount Kenya, Kenya | Kenyte (anorthoclase phonolite) |
This specimen was collected
near Meteorological Station, Mount Kenya, Kenya. It is a coarsely porphyritic
anorthoclase phonolite. It is dominated by large phenocrysts of anorthoclase,
smaller phenocrysts of nepheline, and minor but prominent fayalite crystals.
Mount Kenya is the type locality |
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Specimen# 47-82 | |
Dickson County Kimberlite in thin section |
Dickson County Kimberlite |
Kimberlite, Halas, Dickson County, Michigan, USA | Dickson County Kimberlite prepared slice |
To date, more than 20 distinct
kimberlites have been discovered in Michigan. These post-Ordovician intrusions
range between 20 acres on average and follow a crude northwest trend through
Iron, Dickinson and Menominee Counties. Data obtained from several kimberlites
place them between approximately 186 and 209 ma. While none of the bodies
discovered so far have been proven to be economic, it is believed that many
undiscovered kimberlites exist in the Great Lakes region. Some of these bodies
may be the source of the large historical diamonds found in glacial and
alluvial sediments throughout the midwestern United States. These samples of
kimberlite were found in Hylas, a historic locale, located about three miles
east of Hardwood, in Diskson County, Michigan. It was a station on the Chicago
and North Western Railway Railway, named by the railroad for Hylas from Greek
mythology. The samples are well-rounded similar to river stones and there are
no known kimberlite pipes in the area so an association or locality is unknown.
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Specimen# 48-79 | |
Ugandite thin section not available at this time |
Ugandite |
Ugandite, Indaia II intrusion, Minas Gerais, Brazil | Ugandite |
Indaia consists of two intrusive
plugs, appropriately named Indaia I and II. This is a very fresh ugandite from
Indaia II. It's a sparsely olivine-phyric, fine-grained hypabyssal rock; the
olivine is glassy and entirely fresh. The groundmass is predominatly diopsidic
clinopyroxene with phlogopite, spinel, perovskite, nepheline, and glass! |
|
Specimen# 49-95 | |
Mafic Syenite in thin section |
Surface texture |
Mafic Syenite with igneous compaction. Ice River Complex, British Columbia | Mafic Syenite prepared slice |
Specimen 15-27, described on
catalog page 1, is from the same locality as this syenite but it's from the
other magmatic series. This specimen is a very fresh, medium-grained rock from
the syenite series dominated by nepheline, augite, and amphibole
(kaersutite/barkevikite) with magnetite, apatite, titanite as well as minor
alkali feldspar and sodalite. The nepheline and feldspar are undeformed within
a foliated mat of augite and amphibole probably resulting from compaction near
the solidus. |
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Specimen# 50-72 | |
Fazanda Alagoinha kimberlite in thin section |
Fazanda Alagoinha kimberlite |
Kimberlite, Fazanda Alagoinha | Fazanda Alagoinha kimberlite section |
Kimberlites, the host rock for
diamonds, found in the Fazanda Alagoinha region of Minas Gerais, Brazil, are
transistional between the group I and II kimberlites of South Africa. But
little is known about the kimberlite intrusions in the area because all the
discoveries were done by foreign companies operating in the country. The
groundmass of this specimen is studded with pyrope garnet. |
|
Specimen# 51-70 | |
Olivine Lamproite pyroclastic flow in thin section |
Olivine Lamproite |
Olivine Lamproite pyroclastic flow, Argyle Mine, West Australia, Australia | Olivine Lamproite |
Diamonds occur as sparse
xenocrysts and in mantle xenoliths within olivine lamproite pyroclastic rocks
and dikes. Many deposits are found within funnel-shaped volcanic vents or
craters. Specifically, lamproites are ultrapotassic mafic rocks characterized
by the presence of olivine, leucite, richterite, diopside or sanidine. This
sample is from the Argyle lamproite vent in West Australia, Australia. |
|
Specimen# 52-71 | |
Olivine Melilite hypabassal rock in thin section. |
Olivine Melilite hypabassal rock |
Olivine Melilite hypabassal rock, Howenegg Volcano, Germany | Olivine Melilite |
From the intrusive core of the
Howenegg Volcano, this specimen is very fresh, with glassy phenocrysts of
olivine. The mineralogy includes clinopyroxene, melilite, nepheline, magnetite,
also traces of perovskite, biotite, and spinel. |
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Specimen# 53-73 | |
Alnoite, Hicks Dome in thin section |
Alnoite, Hicks Dome |
Alnoite, Hicks Dome, Southern Illinois, USA | Alnoite, Hicks Dome |
The oldest rocks of the Herod
quadrangle, in Pope, Hardin, Saline, and Gallatin County, Illinois, USA, are
Devonian at the apex of Hicks Dome, an uplift that resulted from Permian
igneous activity and is related to a crypto-volcanic event that produced
pipe-shaped diatremes. Radiometric dating indicates early Permian of about 270
Ma. years ago. Alnoite carbonatite rock consists of melilite, biotite,
pyroxene, calcite, and olivine. Feldspar is not present in the rock, its place
being taken by the mineral melilite. The type location for this rock is
Alnö island off the coast of Sweden. |
|
Specimen# 54-75 | |
Eclogite, Syros, Cycladic Islands in thin section |
Eclogite, Syros, Cycladic Islands |
Eclogite, Syros, Cycladic Islands, Aegean Sea, Greece | Eclogite, Syros, Cycladic Islands |
All eclogites from Syros are
very attractive rock assemblages. They are almost exclusively limited in
distribution to mafic complexes near the middle of the island. Samples are
typically coarse-grained, massive, omphacite-rich rocks with assemblages that
vary from omphacite-garnet-epidote-phengite to
omphacite-garnet-epidote-glaucophane, with minimal amounts of rutile, titanite
and quartz. Chlorite occurs as a common retrograde mineral and apatite occurs
as an accessory mineral. |
|
Specimen# 55-101 | |
Harzburgite, Hokkaido Island in thin section |
Harzburgite, Hokkaido Island |
Harzburgite, Hokkaido Island, Japan | Harzburgite, Hokkaido Island |
This is a rare specimen from the
Horoman peridotite body, Samani-cho, Samani-gun, Hidaka Province, Hokkaido
Island, Japan It's a sample of a complex, layered, peridotite body with a
harzburgite/Iherzolite emplacement related to oceanic mantle, subsided to
deeper mantle depth, before crustal ascension and emplacement (23 Ma). |
|
Specimen# 56-103 | |
Eclogite, Robert Victor Diamond Mine thin section |
Surface texture, Eclogite, Robert Victor Diamond Mine. |
Eclogite, Robert Victor Diamond Mine, South Africa | Prepared slice, Eclogite, Robert Victor Diamond Mine. |
Roberts Victor Mine, Boshof,
Free State Province, South Africa. Located about 40 km east of Boshof it's a
diamond mine in a kimberlite deposit consisting of two dykes, one of which is
associated with two pipes. The diamond grades and qualities of the different
kimberlite bodies varied considerably. In general, diamonds from the pipes were
of poorer quality than those from the dykes. Some parts of the latter contained
diamonds of exceptional quality. This is eclogite from one of the dykes. |
|
Specimen# 57-105 | |
Boar's Tusk Kimberlite in thin section |
Boar's Tusk Kimberlite. |
Kimberlite, Boars Tusk, Wyoming, USA | Boar's Tusk Kimberlite. |
Boars Tusk forms a prominent
volcanic neck of wyomingite (phlogopite-leucite-lamproite) rising 300 feet
above the valley floor. The neck is an agglomerate with abundant xenoliths and
breccia fragments of lamproite. This kimberlite was found at the base. |
|
Specimen# 58-106 | |
Olivine Melilite hypabyssal rock, Mahlberg Castle in thin section |
Olivine Melilite hypabyssal rock, Mahlberg Castle |
Olivine Melilite hypabyssal rock, Mahlberg Castle, near Freiburg, Germany | Olivine Melilite hypabyssal rock, Mahlberg Castle |
The Mahlberg castle is built on
top of a volcanic neck composed of this melilite. The only outcrop is in the
basement of the castle. Olivine melilites are extremely rare rocks. This one is
exceptionally fresh and very dense with glassy phenocrysts of olivine. Also
contains phenocrysts of melilite and clinopyroxene with groundmass perovskite.
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Specimen# 59-107 | |
Wollastonite urtite in thin section |
Wollastonite urtite |
Wollastonite urtite, Ice River Complex, British Columbia, Canada. | Wollastonite urtite |
This is an evolved ijolite with
a large volume of nepheline and lesser amounts of titanite, melanite garnet,
sodic clinopyroxene, and primary wollastonite. Rare, rare, rare! |
|
Specimen# 60-108 | |
On-Line Catalog Page 3
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