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Aktualny stan badań nad meteorytem Morasko

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Muszyński A., Karwowski Ł., Kryza R., Pilski A. S.
Acta Societatis Metheoriticae Polonorum
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2011
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vol. 2
191
2
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Polimineralne nodule w gruboziarnistym meteorycie Morasko

100%
Karwowski Ł., Muszyński A., Kryza R., Pilski A. S.
Acta Societatis Metheoriticae Polonorum
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2009
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vol. 1
52-58
EN
Morasko meteorite (IAB octahedrite) contains numerous graphite-troilite inclusions. Within these inclusions, many mineral phases have been found, including native elements, sulphides, tellurides, oxides, phosphates and silicates. Apart from dominant graphite and troilite, the following minerals occur: copper, sphalerite, daubreelite, chromite, cosmochlor, enstatite, albite and orthoclase; phosphates (buchwaldite and brianite) are found occasionally, whereas djerfischerite, altaite, olivine and silica are rare. The mineral composition of the nodules suggests a more complex origin of the Morasko-type meteorites than currently assumed.
3
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Klasyfikowanie chondrytów zwyczajnych – kolejność prac, metody badań, sprawy formalne i inne problemy

100%
Przylibski T. A., Kryza R., Pilski A. S.
Acta Societatis Metheoriticae Polonorum
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2011
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vol. 2
195-196
4
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Reklasyfikacja meteorytu Pułtusk

100%
Pilski A. S., Karwowski Ł., Siemiątkowski J.
Acta Societatis Metheoriticae Polonorum
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2011
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vol. 2
194
5
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Badania chemiczne deszczu meteorytów żelaznych Jankowo Dolne-Morasko-Przełazy

100%
Pilski A. S., Karwowski Ł., Kryza R., Muszyński A.
Acta Societatis Metheoriticae Polonorum
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2012
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vol. 3
157-158
6
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Nowe znaleziska w rezerwacie „Meteoryt Morasko”

88%
Muszyński A., Pilski A. S., Karwowski Ł., Kryza R., Gurdziel A.
Acta Societatis Metheoriticae Polonorum
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2013
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vol. 4
136-138
7
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Pierwiastki syderofilne w meteorytach Morasko

88%
Pilski A. S., Kryza R., Wasson J. T., Muszyński A., Karwowski Ł.
Acta Societatis Metheoriticae Polonorum
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2012
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vol. 3
62-70
EN
Sixteen specimens of the Morasko, one specimen of Seeläsgen and one specimen of Jankowo Dolne irons were analyzed with INAA to determine contents of 14 siderophile elements. The samples selected for analyses have their structures described and the presence or absence of cohenite checked. For preliminary interpretation, we have chosen elements determined with highest accuracy: Co, Ni, Ga, As, Ir and Au. The results are shown in tables and diagrams. It has been found that there are no significant differences in composition between fragments with and without cohenite. The observed low contents if iridium are not accompanied by lower contents of elements showing similar behavior during crystallization: platinum and tungsten, which suggests that fractional crystallization was not the reason of lower iridium content. Similar concentrations of elements have been found in all the Morasko specimens, and in the Seeläsgen and Jankowo Dolne irons, which suggests that all these meteorites come from one iron shower.
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