Палеозойский вулканизм Днестровско-Прутского междуречья и его отражение в рельефе
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ГРЕБЕНЩИКОВ, В, NEAGA, Vasile, РОМАНОВ, Леонид. Палеозойский вулканизм Днестровско-Прутского междуречья и его отражение в рельефе . In: Buletinul Institutului de Geologie şi Seismologie al AŞM, 2007, nr. 1, pp. 52-57. ISSN 1857-0046.
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Buletinul Institutului de Geologie şi Seismologie al AŞM
Numărul 1 / 2007 / ISSN 1857-0046

Палеозойский вулканизм Днестровско-Прутского междуречья и его отражение в рельефе

Pag. 52-57

Гребенщиков В1, Neaga Vasile2, Романов Леонид2
 
1 Приднестровский Государственный Университет им. Т.Г.Шевченко,
2 Институт геологии и сейсмологии АНМ
 
 
Disponibil în IBN: 29 noiembrie 2013


Rezumat

Volcanogenic Rocks typical for the platform deposits magmatism have been penetrated by boreholes drilled in the south of Dniester-Prut interfluve. The outflow centers are presented by ring structures and associated with Arciz Frunsovka through fault. The deposits are less developed in Transprut zone. Recoverable oil and gas deposits are associated with ledge formations occurring at volcanoes sides.

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<dc:creator>Grebenşcicov, V.P.</dc:creator>
<dc:creator>Neaga, V.I.</dc:creator>
<dc:creator>Romanov, L.F.</dc:creator>
<dc:date>2007-05-01</dc:date>
<dc:description xml:lang='en'>Volcanogenic Rocks typical for the platform deposits magmatism have been penetrated by
boreholes drilled in the south of Dniester-Prut interfluve. The outflow centers are presented by
ring structures and associated with Arciz Frunsovka through fault. The deposits are less developed
in Transprut zone. Recoverable oil and gas deposits are associated with ledge formations
occurring at volcanoes sides.
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<dc:source>Buletinul Institutului de Geologie şi Seismologie al AŞM  (1) 52-57</dc:source>
<dc:title>Палеозойский вулканизм Днестровско-Прутского междуречья и его отражение в рельефе
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