The structure of the Moldovan iron ore deposit (The Ukrainian shield) according to geological-geophysical data and its possible endogenous nature
© V.A. Entin, O.B. Gintov, S.V. Mychak, A.A. Yushin, 2015
An idea of the endogenous nature of ferriferous and ferriferous-carbonate rocks, forming numerous relatively small size of deposits
and ore manifestations in the region of the Middle Bug area called Pobuzhsky iron-ore district has been expressed on the example of the
Moldovan iron-ore deposit (Middle Bug area, Ukraine). This representation is an alternative for the most commonly held view of the s
edimentary-volcanogenic metamorphic origin of iron ore deposits in the Ukrainian Shield the rocks of which are collected in tight folds
with subvertical wings and subhorizontal hinges.
As a proof of endogenous nature of the Moldovan deposit the results of complex interpretation of magnetic and gravity surveys at a scale
of 1:2000-1:5000, the study of physical properties of rocks and deep drilling (1200 m), which indicate the subvertical drop in ore deposits,
a completelack of even the initial signs of folding of total collapse and centriclinal or periclinal locking in the structure of deposits have been given
in this article. The preliminary isotope analysis of carbonate rock deposits also showed a trend of their composition toward carbonatites.
It is shown that the deposit is a hook-like drag fold with vertical hinge formed, as supposed, from iron-ore dyke at length of 2-3 km and
complicated in the hinge part of the impact of volcanic extrusion. These dykes of ferriferous rocks and ores are known in many regions of the world.
Key words: Middle Bug area, Moldovan iron ore deposit, magmatism, structure, genesis.