Submit an Article
Become a reviewer
Vol 55 Iss. 2
Pages:
17-18
Download volume:
RUS
Article

Fauna from the iron ore pit of the Sarbaiskoye deposit

Authors:
S. N. Guseva
V. G. Lazarenkov
Date submitted:
1967-08-18
Date accepted:
1967-10-16
Date published:
1968-08-15

Abstract

The deposit lies among dislocated and metamorphosed sedimentary-volcanogenic rocks of Paleozoic age (Valerian Formation), which have a monoclinal bedding with a westward dip at an angle of 40 45°. The deposit consists of three stratiform ore bodies occurring conformably with volcanogenic-sedimentary rocks: Western, Eastern and Southeastern. The age of the ore bearing strata of the Sarbaiskoye deposit has so far been determined by foraminifera from the core of the well located near the Western ore body (Middle Upper Visean Lower Namurian). Our faunal discovery belongs to the tuffite horizon composing the hanging wall of the Eastern ore body. ...

Область исследования:
(Archived) Without section
Funding:

None

Go to volume 55

Similar articles

On the methodology of operational exploration at the Pikalevskoye deposit
1968 B. I. Laskatelev, P. D. Muzychenko
On the geological structure of the Sarbaiskoye deposit
1968 A. I. Moskalenko
Regularities of crystal nests location distribution within one of the Ural crystal-bearing line fields of the Urals.
1968 V. D. Nikitin, S. A. Rudenko, V. Yu. Eshkin
Hydrothermal changes in carbonate rocks near quartz bodies and crystal nests (on the example of one of the Urals rock crystal deposits) of the Urals).
1968 A. I. Bochkarev
On tectonic control of sulfide mineralization at the Sokolovskoye deposit
1968 V. G. Lazarenkov
Some features of formation of hydrothermally altered rocks of volcanogenic areas (propylites, secondary quartzites) and their prospecting significance
1968 S. V. Sendek