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Clays and Clay Minerals; December 2005; v. 53; no. 6; p. 639-652; DOI: 10.1346/CCMN.2005.0530610
© 2005 Clay Minerals Society
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COMPOSITIONAL AND STRUCTURAL VARIATION OF SUDOITE FROM THE BETIC CORDILLERA (SPAIN): A TEM/AEM STUDY

María Dolores Ruiz Cruz1,* and Carlos Sanz de Galdeano

1 Departamento de Química Inorgánica, Cristalografía y Mineralogía, Facultad de Ciencias, Campus de Teatinos, Universidad de Málaga, Spain
2 Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de Granada, Facultad de Ciencias, 18071 Granada, Spain

* E-mail address of corresponding author: mdruiz{at}uma.es

Sudoite from diagenetic to very low-grade metaclastites of the Betic Cordillera was studied by X-ray diffraction and transmission/analytical electron microscopy. Sudoite formed directly from dickite, the assemblage dickite + sudoite + illite being replaced at increasing metamorphic grade by the assemblage pyrophyllite + sudoite + illite. Sudoite ranges in composition from Mg-rich to Fe-rich chemistries. In addition, a wide variety of mixed-layered structures (illite-sudoite, pyrophyllite-sudoite, and dickite-sudoite) was also identified. Mg-rich sudoite shows a mean chemical composition of (Al2.91Fe2+ 0.25Mg1.80)(Si3.10Al0.90)O10(OH)8, and a IIb ordered structure with b = 9.055 Å. Intermediate Fe-Mg sudoite exhibits a very variable composition, the Fe-rich phases having a mean composition of (Al2.09Fe3+ 0.61Fe2+ 0.87Mg1.44)(Si3.31Al0.69O10(OH)8. These are disordered polytypes with b values ranging from 9.070 to 9.101 Å. Fe occurs in both octahedral sheets, according to two types of substitutions: Fe3+ for Al in the dioctahedral sheet and Fe2+ for Mg in the trioctahedral sheet. Sudoite with such a composition has not been described previously.

Key Words: Betic Cordillera • Dickite • Illite • Mixed-layer • Pyrophyllite • Spain • Sudoite




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