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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Southern Europe
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Italy
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Sicily Italy
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Catania Italy (2)
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Hyblean Plateau (1)
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Mount Etna (7)
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Mediterranean Sea
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East Mediterranean
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Ionian Sea (1)
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elements, isotopes
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isotope ratios (1)
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isotopes
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radioactive isotopes
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Ra-226 (1)
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Th-230 (1)
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Th-230/Ra-226 (1)
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metals
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actinides
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thorium
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Th-230 (1)
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Th-230/Ra-226 (1)
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alkaline earth metals
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radium
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Ra-226 (1)
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Th-230/Ra-226 (1)
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geochronology methods
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Ar/Ar (2)
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K/Ar (1)
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paleomagnetism (2)
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Th/U (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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lower Holocene (1)
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upper Holocene
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Roman period (1)
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Pleistocene
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upper Pleistocene (1)
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igneous rocks
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igneous rocks
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volcanic rocks
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basalts (2)
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pyroclastics (1)
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Primary terms
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absolute age (3)
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academic institutions (1)
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biography (2)
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Cenozoic
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Quaternary
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Holocene
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lower Holocene (1)
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upper Holocene
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Roman period (1)
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Pleistocene
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upper Pleistocene (1)
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continental drift (1)
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earthquakes (1)
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Europe
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Southern Europe
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Italy
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Sicily Italy
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Catania Italy (2)
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Hyblean Plateau (1)
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Mount Etna (7)
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-
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faults (1)
-
geochronology (2)
-
geomorphology (3)
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geophysical methods (1)
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igneous rocks
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volcanic rocks
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basalts (2)
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pyroclastics (1)
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-
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isotopes
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radioactive isotopes
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Ra-226 (1)
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Th-230 (1)
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Th-230/Ra-226 (1)
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lava (1)
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magmas (2)
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Mediterranean Sea
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East Mediterranean
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Ionian Sea (1)
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-
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metals
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actinides
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thorium
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Th-230 (1)
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Th-230/Ra-226 (1)
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-
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alkaline earth metals
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radium
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Ra-226 (1)
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Th-230/Ra-226 (1)
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paleomagnetism (2)
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petrology (2)
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plate tectonics (2)
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remote sensing (1)
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sedimentation (1)
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tectonics
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neotectonics (2)
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volcanology (2)
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sedimentary rocks
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volcaniclastics (1)
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sediments
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volcaniclastics (1)
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ABSTRACT We present an interdisciplinary study between philosophy and science that uses a historical case to show some aspects of scientific research. The case in question is that of Alfred F. Rittmann (1893–1980), known as one of the central figures of twentieth-century volcanology. After outlining Rittmann’s scientific background and hypotheses, we briefly examine the set of his theories using Thomas Kuhn’s model of the development of science. We highlight the methodology of multiple working hypotheses and how they contributed to defining his geoscientific paradigm, namely, magmatological tectonics. Rittmann worked on his paradigm throughout his life, even making little-known criticisms on plate tectonics. We present some of them, contextualizing them in twentieth-century as well as current research. His use of multiple working hypotheses, along with his drive to search for synthetic visions between different models, could be a stimulating and pluralistic approach to unsolved geoscientific questions.