Geneza rewolucji naukowej w geologii

Marzena Dybkowska

Marzena Dybkowska Biblioteka Uniwersytecka KUL

Słowa kluczowe: teoria płyt litosfery, rewolucja naukowa w geologii, metodologia geologii

Abstrakt

The genesis of plate tectonics was the beginning of the scientific revolution in geology. Due to the analysis in Kuhn's terminology some elements in this revolution are able to be shown. The stabilist paradigm was replaced by the mobilist one as a consequence of changing ontological presuppositions assumed in geology. Essential new information was provided by scientific discoveries in oceanography and paleomagnetism. In connection with that a growing crisis in the stabilist paradigm took place. The explaining hypotheses, for instance the hypothesis of sea-spreading and Vine-Matthews hypothesis, came into being. Next they were united into plate tectonics. The consensus among geologists appeared also indispensable. It included a reception of the new theory in the late 1960s and an acceptance of the scientific change that was revolutionary in its character.

Bibliografia

Cwojdziński S.: Dokąd zmierza współczesna geotektonika?, „Przegląd Geologiczny”, 32(1984), nr 10, s. 505-513.

Czechowski L.: Tektonika płyt i konwekcja w płaszczu Ziemi, Warszawa: PWN 1994.

Emiliani C.: Two Revolutions in the Earth Sciences, „Terra Nova”, 7(1995), No. 6, s. 587-597.

Giere R. N.: Explaining Science: A Cognitive Approach, Chicago−London 1988.

Hallam A.: A Revolution in the Earth Sciences: From Continental Drift to Plate Tectonics, Oxford: Clarendon Press 1973.

Jacoby W. R.: Modern Concepts of Earth Dynamics Anticipated by Alfred Wegener in 1912, „Geology”, 9(1981), No. 1, s. 25-27.

Jones B.: Plate Tectonics: A Kuhnian Case?, „New Scientist”, 63(1974) 536-538.

Mała Encyklopedia Filozofii. Pojęcia, Problemy, Kierunki, Szkoły, Bydgoszcz: Branta 1996.

VanAndel T. H.: Nowe spojrzenie na starą planetę. Zmienne oblicze Ziemi, tł. z jęz. ang. W. Studencki, Warszawa: PWN 1997.