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This mineral deposit may properly be divided into two parts, the bed or floor, and
the hamm, as it is here called, or overlier. The latter consists of a more or less
distinct aggregate of chert, quartz, hornblende, chlorite and actinolite.
Royal Geological Society of Cornwall,
1822
2
Transactions of the Royal geological Society of Cornwall
This mineral deposit may properly be divided into two parts, the bed or floor, and
the kamm, as it is here called, or overlier. Thelatter consists of a more or less
distinct aggregate of chert, quartz, hornblende, chlorite and actinolite. Some
portions ...
3
TRANSACTIONS OF THE ROYAL GEOLOGICAL SOCIETY OF CORNWALL
This mineral deposit may properly be divided •into two parts, the bed or floor, and
the kamm, as it is here called, or overlier. The latter consists of a more or less
distinct aggregate of chert, quartz, hornblende, chlorite and actinolite.
ROYAL GEOLOGICAL SOCIETY,
1822
1979). The cyclical character of sediments disappears toward the stratigraphic
overlier. Permian sediments are not yet biostratigraphically divided in detail. They
are light-coloured. coarse-sandy and fine-conglomeratic, without distinct cyclical
...
Instituto Geológico y Minero de España, J. L. Escobedo,
1985
5
Transactions of the Royal Geological Society of Cornwall
This mineral deposit may properly be divided into two parts, the bed or floor, and
the hamm, as it is here called, or overlier. The latter consists of a more or less
distinct aggregate of chert, quartz, hornblende, chlorite and actinolite.
Royal Geological Society of Cornwall,
1818
6
Triassic Foraminifers of the West Carpathians
In its overlier are local light bank, partly brecciated limestones (Dachstein
limestones) and then the Kössen Member. Since the Dachstein limestones and
the Kössen Member are on the surface only at scarce localities on the northern
slope of ...
Jozef Salaj, Karol Borza, Ondrej Samuel,
1983
7
Geologické práce: Zprávy
(1) Hyaloclastite breccia in the overlier of the lava flows The hyaloclastite breccia
situated in the overlier of the flows and bound to them by gradual transition,
represents a product of disintegration of the upper part of the flow on the contact
with ...
8
18th European Colloquy on Micropaleontology: Excursion ...
Stratigraphical range: Aalenian - Middle Bajocian. The Super-Posidonia
Formation It is in the overlier of the Posidonia Formation. It consists of medium
and thick-bedded dark-grey, brown-grey, brown and black limestones with dark
spots.
Ondrej Samuel, Viera Gašparíková,
1983
The age of this metallogenetic stage is estimated to be Lower Devonian (overlier
of the lydite and carbonate horizons). The lower ore-bearing horizon can be
followed everywhere in those places where there is a developed lower
variegated ...
10
Geologický zborník: Geologica Carpathica
They ascribed a Ladinian age to the Reifling Limestones, parallelizing the shaly
sequences in their overlier with the Lunz beds. Borza (1970) was dealing with
more detailed stratigraphy of the lower part of the "Reifling Limestones".
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SLO County enhances Paso groundwater management
The Paso Robles Basin Water District, proposed as a joint plan agreement between two overlier groups—Paso Robles Agriculture Alliance for ... «New Times SLO, 三月 14»
Two lawsuits and an agreement complicate the stabilization of the …
Some agriculturalists have expressed concerns of more bureaucracy and a threat to private property rights and the associated overlier rights. «New Times SLO, 十二月 13»