M. Garecka

发表

Paleogene microfossils from the submarine debris flows in the Skole basin (Polish and Ukraine Outer Carpathians)

L. Jankowski, A. Szydło, M. Garecka, 2014 .

Radio-isotopic age and biostratigraphic position of a lower Badenian tuffite from the western Polish Carpathian Foredeep Basin (Cieszyn area)

K. Kuiper, K. Bukowski, M. Garecka, 2018 .

Lower Oligocene Menilite Beds, Polish Outer Carpathians: supposed deep-sea flysch locally reinterpreted as shelfal, based on new sedimentological, micropalaeontological and organic-geochemical data

A. Szydło, M. Garecka, I. Matyasik, 2016 .

The position and age of flysch deposits in the Crimean Mountains (Southern Ukraine)

N. Oszczypko, A. Ślączka, B. Olszewska, 2017 .

Analysis of reworked sediments as a basis of the Palaeogene-Neogene palaeogeography reinterpretation: Case study of the Roztocze region (SE Poland)

L. Jankowski, W. Margielewski, J. Urban, 2017 .

The po si tion and age of flysch de pos its in the Cri mea Moun tains ( South ern Ukraine )

N. Oszczypko, A. Ślączka, B. Olszewska, 2017 .

Fossil karst in the Jurassic of Kościuszko Mound in Kraków (southern Poland)

A. Wójcik, B. Olszewska, M. Garecka, 2014 .

Calcareous nannoplankton from the Podhale Flysch (Oligocene-Miocene, Inner Carpathians, Poland)

M. Garecka, 2005 .

Record of changes in the Oligocene–Miocene sediments of the Menilite–Krosno series of the Skole Unit based on calcareous nannoplankton studies – biostratigraphy and palaeogeographical implications (Polish Outer Carpathians)

M. Garecka, 2012 .

Correlation of the Middle Miocene deposits in SE Poland and western Ukraine based on foraminifera and calcareous nannoplankton

B. Olszewska, M. Garecka, 2011 .

Biostratigraphy of the Early Miocene of the Southern Poland based on planktic foraminifera and calcareous nannoplankton

B. Olszewska, M. Garecka, 1998 .

Calcareous nannofossils and foraminifera from the youngest deposits of the Siary Subunit (Oligocene, Magura Nappe, Polish Outer Carpathians)

A. Szydło, M. Garecka, 2015 .