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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Morocco
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Rif (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Western Europe
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elements, isotopes
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igneous rocks
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ultramafics
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metamorphic rocks
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minerals
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halides
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silicates
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chain silicates
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pyroxene group
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orthosilicates
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sorosilicates
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epidote group
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allanite (1)
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sheet silicates
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chlorite group
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cookeite (3)
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clay minerals
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kaolinite (1)
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mica group
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paragonite (1)
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Primary terms
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Africa
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North Africa
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Morocco
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Rif (1)
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atmosphere (1)
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bibliography (1)
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Cenozoic
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Tertiary
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Neogene
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Paleogene
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crystal chemistry (2)
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diagenesis (1)
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Europe
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Southern Europe
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Iberian Peninsula
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Portugal (1)
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Spain
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Andalusia Spain
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Alpujarride Complex (1)
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Nevado-Filabride Complex (1)
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Serrania de Ronda (1)
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Betic Cordillera
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Serrania de Ronda (1)
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Cameros Basin (1)
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Western Europe
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Scandinavia
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Norway
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Nordland Norway (1)
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geochemistry (1)
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igneous rocks
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plutonic rocks
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granites
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aplite (1)
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pegmatite (2)
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ultramafics
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peridotites (1)
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mantle (1)
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Mediterranean region (1)
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Mesozoic
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Triassic (1)
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metals
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rare earths
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cerium (1)
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yttrium (1)
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metamorphic rocks
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metasedimentary rocks
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metapelite (1)
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metamorphism (3)
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orogeny (1)
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plate tectonics (1)
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weathering (1)
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saliotite
La saliotite, interstratifie regulier 1:1 cookeite/paragonite; nouveau phyllosilicate du metamorphisme de haute pression et basse temperature
Polytypism of cookeite in low-grade metapelites of the Cameros Basin, Spain: Lack of correlation of well-ordered polytypes with pressure
Clay minerals in the Namacotche Pegmatite Group from Zambezia Province, Mozambique: main constituents of late-stage secondary paragenesis
Perbøeite-(Ce) and alnaperbøeite-(Ce), two new members of the epidote-törnebohmite polysomatic series: Chemistry, structure, dehydrogenation, and clue for a sodian epidote end-member
Lateral variations of pressure-temperature evolution in non-cylindrical orogens and 3-D subduction dynamics: the Betic-Rif Cordillera example
ALTERATION OF SPODUMENE TO COOKEITE AND ITS PRESSURE AND TEMPERATURE STABILITY CONDITIONS IN Li-BEARING APLITE-PEGMATITES FROM NORTHERN PORTUGAL
Clay mineral evolution
Abstract Micas and other phyllosilicates are important recorders of metamorphic processes and reaction progress. The presence of sheet silicates in the lowest diagenetic grade, through higher metamorphic zones, to anatexis allows for the continuous monitoring of physico-chemical changes during metamorphism. Their fine-grained nature, and their penchant for mixing on very small scales, makes the use of transmission electron microscopy (TEM) essential for detailed crystal-chemical examinations and determinations of chemical compositions. This chapter outlines the advances in our understanding of low-grade metamorphism, deformation and intergrowths in micas and some related phyllosilicates, that have benefited from TEM studies. Particular attention is paid to low-grade metamorphism and then to selected studies illustrating the value of TEM.