Wyniki wyszukiwania - AGRO

1

Anna Sadowska. March 20, 1937 - October 10, 2005

100%

Kuszell T., Malkiewicz M.

Geologia Sudetica

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2005

|

tom 37

2

Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik

Remembrance of Antoni Hoffman

100%

Kielan-Jaworowska Z.

Acta Palaeontologica Polonica

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1993

|

tom 38

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nr 3-4

3

3rd Meeting of the Czech Tectonic Studies Group [Ceska Tektonicka Skupina], Mala Upa, Czech Karkonosze Mts, April 15-19, 1998

100%

Puziewicz J.

Geologia Sudetica

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1998

|

tom 31

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nr 1

4

Mesostructural and kinematic characteristics of core gneisses in western part of the Orlica-Snieznik Dome, West Sudetes

100%

Dumicz M.

Geologia Sudetica

|

1998

|

tom 31

|

nr 1

5

The methodology of magnetotelluric investigation in heterogeneous media

100%

Miecznik J., Stefaniuk M., Klitynski W.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1995

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tom 43

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nr 2

6

Quaternary geology at Lions Rump [SSSI No.34], King George Island, South Shetland Islands [West Antarctica]

100%

Birkenmajer K.

Bulletin of the Polish Academy of Sciences. Earth Sciences

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1994

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tom 42

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nr 3

7

Petrography and depositional conditions of the coal seams of the Walbrzych Formation, Intrasudetic Basin, SW Poland

100%

Mastalerz M.

Geologia Sudetica

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1992

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tom 26

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nr 1-2

8

EUROBRIDGE - The 7th Working Meeting, Suwalki-Szelment, May 26th-30th, 1999

100%

Lorenc M. W., Wiszniewska J.

Geologia Sudetica

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1999

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tom 32

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nr 1

9

The 12th meeting of the Petrology Group of the Mineralogical Society of Poland "Crystalline Rocks of the East-European Craton" Stary Folwark, 13-16 October 2005

86%

Ilnicki S.

Geologia Sudetica

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2005

|

tom 37

10

A flashback on the dawn of the meteorite impact/extinction theory

86%

Smit J.

Acta Palaeontologica Polonica

|

2012

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tom 57

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nr 4

Presented are my personal recollections on some of the major contributions by the Alvarez groups to the birth and development of the meteorite impact/extinction theory.

11

Can the soil geology and chemistry analysis of a site predict the geographic origin of wild edible mushrooms (Porcini group)?

86%

Ambrosio E., Marescotti P., Benucci G. M. N., Cecchi G., Brancucci M., Zotti M., Mariotti M. G.

Acta Mycologica

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2019

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tom 54

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nr 2

12

The 3rd meeting of the Central European Tectonic Group and the 10th meeting of the Czech Tectonic Studies Group, Felsotarkany, Hungary, April 14-17, 2005

86%

Jastrzebski M., Murtezi M.

Geologia Sudetica

|

2005

|

tom 37

13

The 2nd meeting of the Central European Tectonic Group and 9th meeting of the Czech Tectonic Studies Group, Lucenec, Slovakia, June 22–25, 2004

86%

Jastrzebski M., Murtezi M.

Geologia Sudetica

|

2005

|

tom 37

14

W kraju i w świecie (kartki z życiorysu)

86%

Birkenmajer K. L.

Analecta. Studia i Materiały z Dziejów Nauki

|

2011

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tom 20

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nr 2

15

Structural geology of the Basement Complex rocks in Iwaraja area, southwestern Nigeria

86%

Adeoti B., Okonkwo C. T.

International Letters of Natural Sciences

|

2016

|

tom 58

The geological and structural evolution assessment of the Basement Complex rocks in Iwaraja area, southwestern Nigeria showed that the basement rocks comprise quartzites and quartzschists of the Effon Psammite Formation, quartz-mica schists, biotite schists, migmatitic gneisses, granitic gneisses, late and post-tectonic granitic rocks including pegmatites, which have been subjected to two phases of deformation. The first phase is mainly a fabric forming deformation that also led to the development of moderately plunging mineral lineation. No minor fold of this phase was recognized. The second deformation phase gave rise to the development of Iwaraja (ductile) shear zone. The mylonitic foliation is sub-vertical and steeply dipping and while the mineral lineation is sub-horizontal and shallowly plunging. Within granitic gneiss mylonites, the shear zone is characterised by early and late open to tight folds of pegmatite dykes. Adjacent the shear zone, ptygmatic folds of quartzo-feldspathic veins in gneisses and crenulated cleavages that overprinted earlier schistosity surfaces in the quartz-mica schist also characterised this deformation phase. Extensional fractures in the various lithologies generally show bimodal orientations mainly in the WNW-ESE and NW-SE directions, which are nearly perpendicular to the regional metamorphic foliations. These deformation conditions depict structural features that are associated with internal zones of orogenic belts. Within the study area, the structures document late-Precambrian deformation during the closing stages of Pan-African orogenesis.

16

K-Ar dating of the Miocene andesite intrusions, Pieniny Mts, West Carpathians, Poland

86%

Birkenmajer K., Pecskay Z.

Bulletin of the Polish Academy of Sciences. Earth Sciences

|

1999

|

tom 47

|

nr 2-3

17

Inherited landforms in the crystalline areas of the Sudetes Mts. A case study from the Jelenia Gora Basin, SW Poland

86%

Migon P.

Geographia Polonica

|

1992

|

tom 60

18

EUG 10: The European Union of Geosciences Meeting, Strasbourg, March 28 - April 1, 1999

86%

Kryza R.

Geologia Sudetica

|

1999

|

tom 32

|

nr 1

19

Ecological aspects of sedimentology. 7th National Meeting of Sedimentologists, Wojcieszow, July 2-4, 1998

86%

Raczynski P.

Geologia Sudetica

|

1999

|

tom 32

|

nr 1

20

International Conference: Orogenic Processes - Quantification and Modelling in the Variscan Belt, Freiberg, Saxony, February 22-26, 1999

86%

Aleksandrowski P.

Geologia Sudetica

|

1999

|

tom 32

|

nr 1

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