4. C z e c z 0 t t H. - 0 wieku trzeciorzl;dowej fiary Turowa k. Bogatyni (G6rne l..tiZyce). Kwart. geol., 1970, nr 4.
5. F ran ci s W. - Coal, Its formation and com-position. London, 1954.
6. Got h an W. - Autochtonie und Allochtonie bei der Braunkohle. Zschr. f. prakt. Geo!., Halle, 1930. Jg. 38, H.5.
7. Hun g erR. - Mikrobotanisch-stratigraphische UntersuchuIigen der Braunkohlen der sUdlichen Oberlausitz und die Pollenanalyse als Mittel zur Deutung der F18zgenese, Freib. Forsch., C. H. 8, Geologie, Berlin, 1953.
8. J u n g W. - Neue paUii>bDtanische Untersu-chungen an den Braunkohlen der Oberpfalz. Ber. Bayer. Bot. Ges., 1972, Bd 43.
9. Jung W., KnoblDch E., Kivacek Z. -Makrofloristische Untersuchungen im
Braunkoh-lenterWir der Oberpfalz. 'Mitt. Bayer.Staats-samml. PaUiont. hist. Geol., MUncben, 1971, H. 11.
10. K r u s z e w ski T. - Badania . petrograficzne wE:gli brunatnych z kopalni Tur6w. T. II, Pr. GIG, Katowice, 1964.
11. K sI,,:! k i e w I c
z
M. - Geologia dynamiczna. Wyd. 4, Wyd. Geot, 1972.SUMMARY
The hypothesis of autochtoneous origin of coal
in result of alteration of peats is accepted. Sub-sequently, the author discusses some evidence com-monly put forward by the supporters of the alter-native hypothesis of allochtoneous origin of coals. The arguments given for the latter hypothesis are critically reviewed from the PDint of view of pa-leobotany and using some results of the author's studies on brown coals.
It is concluded that the allochtony proper, ie. primary allochtony, as well as secondary allochto-ny cannot . be considered as of any importance :Cor the origin of coals from the point of view of pa-leobotanists. The two forms of allochtony may par-ticipate in formation of coals only as local phe-nomena of very limited significance. The impor-tance of allochtony for the formation of coals may be accepted only in exceptional cases with good geological record. From the point of view of pa-leobotany it may be accepted. that coals, similarly as peats, may originate under various hYdrological conditions and in various peat-bogs but always au-tochtonically.
18
12. K u I c z y
n
ski S. _ . Geneza karbonskich· zl6z wc:gIowych. Pr. Wrocl. Tow. Nauk., ser. B, Wro-claw, 1952, nr 64.13. K u I c
z
y fl ski S. - Torfowiska PDlesia. T. 1--11. Krak6w, 1939-1940.14. Lubliner-Mianowska K.,
Kw.iatkow-ski A. - Badania nad zaleZn~cill zawarto~ci
substancji woskowo-bitumicznyCh w ' tQrfie od jego sldadu ro~linnego . i stop~ia rozldadu. Zesz ..
nauk. Pol Gd., 1954. .
15. Po s t L. von, G ran 1 u n d E. - Sodra. Sve-riges Torv-tillgangar. Sv; geo~. · Under~., Ser.· C,
Stockholm, 1 9 2 4 . ' .
16. Raistrick A., Marshall C. E . . _ . The nature and origin of coal and coal seams. Lon-don, 1948.
17. S top a S. Z. - Klasyfikacja antrakogenetyczna formacji wE:gIono~nych. Pr. geol. Kom. Nauk. GeoL PAN Oddz. w Krakowie 1968, nr 49.' 18. T h 0 m son P. W. - Pseudo-Allochtonie imd
partielle Autochtonie. Neues Jb. Geo!.. Palaont., Mh., Abt. B, Geol.-Palaont., 1958, H. 6. 19. Tolpa S. - Torfowlska i torfy. Wroclaw
Warszawa, 1949.
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