Fault-hosted palygorskite from the Serrata de Níjar deformation zone (Se Spain)
نویسندگان
چکیده
منابع مشابه
Kinematics of Transpressional Deformation Zones in the Urmia Fault Zone, Northwest Iran
Metamorphic and various intrusive rocks in the Urmia area are located in a transpressed active continental margin. These complexes in the Zagros orogen were deformed during an oblique convergence scenario between the Arabian and Sanandaj–Sirjan blocks in NW Iran. The Urmia area contains both NW-SE striking dextral strike-slip and SW verging NE dipping ductile reverse shear fabrics. Ductile shea...
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M. Chlieh,1,∗ J. B. de Chabalier,1 J. C. Ruegg,1 R. Armijo,1 R. Dmowska,2 J. Campos3 and K. L. Feigl4 1Institut de Physique du Globe de Paris, Départements de Tectonique et de Sismologie, CNRS UMR 7578 & 7580, 4 Place Jussieu, 75252 Paris cedex 05, France. E-mail: [email protected] 2Division of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, USA 3Departamento de ...
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AB STRACT: Glauconite and Ca phosphate peloids occur in Jurassic and Cretaceous bioclastic carbonate rocks from pelagic swell sequences of the Algayat-Crevillente Unit (Subbetic Zone). The size and morphology of the peloids are controlled by the bioclasts. The glauconite in both stratigraphic positions is K rich (>0.69 atoms p.f.u.) and shows well-defined 10 AÊ lattice fringes. Poorly crystalli...
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ژورنال
عنوان ژورنال: Clays and Clay Minerals
سال: 2006
ISSN: 0009-8604,1552-8367
DOI: 10.1346/ccmn.2006.0540304