Works matching IS 14373254 AND DT 2002 AND VI 91 AND IP 1
Results: 12
Active mud volcanoes on- and offshore eastern Makran, Pakistan.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 93, doi. 10.1007/s005310100203
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Hercynian tectono-thermal evolution associated with crustal extension and exhumation of the Lora del Río metamorphic core complex (Ossa-Morena zone, Iberian Massif, SW Spain).
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 76, doi. 10.1007/s005310100206
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Late Visean thermal event in the northern part of the French Massif Central: new <sup>40</sup>Ar/<sup>39</sup>Ar and Rb–Sr isotopic constraints on the Hercynian syn-orogenic extension.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 53, doi. 10.1007/s005310100202
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Organization of pre-Variscan basement areas at the north-Gondwanan margin.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 35, doi. 10.1007/s005310100200
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Peraluminous granites frequently with mantle-like isotope compositions: the continental-type Murzinka and Dzhabyk batholiths of the eastern Urals.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 3, doi. 10.1007/s005310100195
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Constraints on the timing of granite emplacement, deformation and metamorphism in the Shamva area, Zimbabwe.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 20, doi. 10.1007/s005310100198
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Stratigraphic and metamorphic inversions in the central Menderes Massif: a new structural model.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 179, doi. 10.1007/s005310100220
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Late Quaternary ice-rich permafrost sequences as a paleoenvironmental archive for the Laptev Sea Region in northern Siberia.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 154, doi. 10.1007/s005310100205
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Clay mineral sedimentation in high northern latitude deep-sea basins since the Middle Miocene (ODP Leg 151, NAAG).
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 133, doi. 10.1007/s005310100199
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Why did ancient chemosynthetic seep and vent assemblages occur in shallower water than they do today? Comment.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 149, doi. 10.1007/s005310100196
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Paleoenvironmental evolution of the Paratethys in the Slovenian Basin during the Late Paleogene.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 123, doi. 10.1007/s005310000118
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Redbeds from the Middle Muschelkalk (Middle Triassic) of the SW Germanic Basin: arid environments from Pangea's interior.
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- International Journal of Earth Sciences, 2002, v. 91, n. 1, p. 111, doi. 10.1007/s005310100201
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