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Wyświetlanie 1-2 z 2
Tytuł:
Nefryt z Nasławic na Dolnym Śląsku
Nephrite from Nasławice in Lower Silesia (SW Poland)
Autorzy:
Łobos, K.
Sachanbiński, M.
Pawlik, T.
Powiązania:
https://bibliotekanauki.pl/articles/2074569.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
nefryt
serpentynity
rodingity
masyw Gogołów-Jordanów
ofiolit Ślęży
nephrite
serpentinites
rodingites
Ślęża ophiolite
Opis:
During exploitation of serpentinite in the Nasławice quarry (SW Poland) a nephritic zone has been identified. Nephrite occurs in association with light in color rock, similar to rodingite, composed almost entirely of garnet. These rocks form oval bodies in serpentinites. Their maximal length is 7 m and height is 3.5 m. Nephrite appears in the contact zone of one of such bodies. In the upper contact zone nephrite is 10-15 cm thick and in the west side of the rodingite body reaches 40-50 cm. It is possible to distinguish varieties of nephrite from the Nasławice quarry which differ according to color, fabric and mineral composition. Nephrite from Nasławice is hard and reveals splintery fracture. Nephrite is mainly composed of actinolite, which forms fine- grained aggregates (length of fibres ca 100 um) arranged chaotically. Additional minerals also occur such as chromite, garnet enriched in Cr and pyroxene. Microscopic examination reveals that nephrite has massive, fibrous texture. With regard to gemmological properties, three varieties of nephrite have been identified: 1) Homogenous green nephrite with a small amount of chromite inclusions, which cover no more than 5% of surface of sliced samples; 2) Spotted nephrite-with numerous dark spots on a green background; it happens occasionally, that this variety of nephrite changes into serpentinite; 3) Patchy nephrite- characterized by the presence of emerald-green, elongated spots of actinolite (often with grains of chromite inside) on a white background; some fragments contain veins of fibrous serpentine with cat’s eye effect; this seems to be the most interesting sort of nephrite from Nasławice. Based on preliminary technological studies it can be concluded, that nephrite from Nasławice has not only a fine color and interesting texture, visible in sliced samples, but it is also easy for polishing. On polished surfaces nephrite shows fine oily luster. Unfortunately, examples found today are strongly cracked because of the explosive method of serpentinite exploitation used in the Nasławice quarry. The zone of nephrite occurrence is associated with the course of veins of leucocratic rock which extends over a distance of ca 5 km between Nasławice and Jordanów Sląski.
Źródło:
Przegląd Geologiczny; 2008, 56, 11; 991-999
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Struktura prekambryjskiego podłoża wschodniej części bloku górnośląskiego (Brunovistulicum)
Structure of the Precambrian basement of the eastern part of the Upper Silesian block (Brunovistulicum)
Autorzy:
Buła, Z.
Żaba, J.
Powiązania:
https://bibliotekanauki.pl/articles/2074609.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
utwory archaiczno-dolnoproterozoiczne (karelskie)
anchimetamorficzne utwory ediakaru
górnoproterozoiczne utwory krystaliczne
eksternidy i internidy kadomskie
szef ofiolitowy Tychów-Jordanowa
strefa uskokowa Kraków-Lubliniec
fundament Brunovistulicum
Archean-Lower Proterozoic (Karelian) formations
anchimetamorphic Ediacaran formations
crystalline formations of the Upper Proterozoic
Cadomian externides and internides
Tychy–Jordanów ophiolite suture zone
Cracow-Lubliniec fault zone
Brunovistulicum basement
Opis:
Two large, regional tectonic units, represented by Małopolska and Brunovistulicum blocks (terrains) can be distinguished in the southern Poland. The Cracow–Lubliniec fault zone forms their border. They vary both in the structures of the Precambrian basement and the Paleozoic rock cover, which shows different paleogeographic-facies and paleotectonic development. They are separated from the neighboring tectonic units by immense deep fault zones. Archean and Early Proterozoic metamorphic rocks within the Rzeszotary horst (2.6–2.8 and 2.0 Ga) are the oldest formations building the Brunovistulicum basement. Farther to the west, Precambrian and Ediacaran anchimetamorphic siliclastics can be observed. Cadomian-Precambrian rocks (640–545 Ma), which outcrop only near Brno, occur south and west of them. In the western part of the Brunovisitulicum (theWestern Sudetes) Variscan orthogneiss occurs. The age of its protholite varies vastly; from approximately 1020 Ma through 680–570 Ma to approximately 520–500 Ma. Precambrian basement of the Brunovistulicum is heterogenic. Within the area of Poland, it is formed by two fragments of the crust, represented by Karelian and Early Karelian rocks of the Rzeszotary horst and Cadomian crystalline and anchimetamorphic rocks occurring west of Rzeszotary. Between them, two vast, connected together, magnetic maxima in the vicinity of Tychy and Jordanów can be observed in a magnetic field image delta Z. The origin of those anomalies is related to the occurrence of gabbro, diabase and/or ultrabasite (ophiolite) rocks. Referring to the earlier concepts, it may be currently assumed that the anomaly axis Tychy–Jordanów determines the course of the contact zone (ophiolite suture zone) between the two fragments of the crust of different ages, building the basement of Brunovistulicum: the Archean - Lower Proterozoic (Karelian) and the Upper Proterozoic (Cadomian) formations.
Źródło:
Przegląd Geologiczny; 2008, 56, 6; 473-480
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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