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Kautz, Christopher Q., Ryan, Peter C. (2003) The 10 Å to 7 Å halloysite transition in a tropical soil sequence, Costa Rica. Clays and Clay Minerals, 51 (3) 252-263 doi:10.1346/ccmn.2003.0510302

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Reference TypeJournal (article/letter/editorial)
TitleThe 10 Å to 7 Å halloysite transition in a tropical soil sequence, Costa Rica
JournalClays and Clay Minerals
AuthorsKautz, Christopher Q.Author
Ryan, Peter C.Author
Year2003 (June 1)Volume51
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1346/ccmn.2003.0510302Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID147809Long-form Identifiermindat:1:5:147809:3
GUID0
Full ReferenceKautz, Christopher Q., Ryan, Peter C. (2003) The 10 Å to 7 Å halloysite transition in a tropical soil sequence, Costa Rica. Clays and Clay Minerals, 51 (3) 252-263 doi:10.1346/ccmn.2003.0510302
Plain TextKautz, Christopher Q., Ryan, Peter C. (2003) The 10 Å to 7 Å halloysite transition in a tropical soil sequence, Costa Rica. Clays and Clay Minerals, 51 (3) 252-263 doi:10.1346/ccmn.2003.0510302
In(2003, June) Clays and Clay Minerals Vol. 51 (3) Springer Science and Business Media LLC

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Fisher, G. Burch, Ryan, Peter C. (2006) The smectite-to-disordered kaolinite transition in a tropical soil chronosequence, Pacific coast, Costa Rica. Clays and Clay Minerals, 54 (5) 571-586 doi:10.1346/ccmn.2006.0540504
Mitra, Girija Bhushan (2013) Spiral Structure of 7 Å Halloysite: Mathematical Models. Clays and Clay Minerals, 61 (6) 499-507 doi:10.1346/ccmn.2013.0610602
Slansky, Ervin (1985) Interstratification of 10- and 7-Å Layers in Halloysite: Allegra's Mixing Function for Random and Partially Ordered Stacking. Clays and Clay Minerals, 33 (3) 261-264 doi:10.1346/ccmn.1985.0330314
Bobos, Iuliu (2001) Kaolinite to Halloysite-7 Å Transformation in the Kaolin Deposit of SÃo Vicente de Pereira, Portugal. Clays and Clay Minerals, 49 (6) 596-607 doi:10.1346/ccmn.2001.0490609
Siranidi, Eirini, Hillier, Stephen, Chryssikos, Georgios D. (2024) Structure of tubular halloysite-(10 Å) and its transition to halloysite-(7 Å) by infrared spectroscopy and X-ray diffraction. Clays and Clay Minerals, 72. doi:10.1017/cmn.2024.37
Nagasawa, K. (1974) Artificial Alteration of Biotite into a 14 Å Layer Silicate with Hydroxy-Aluminium Interlayers. Clays and Clay Minerals, 22 (3) 241-252 doi:10.1346/ccmn.1974.0220306
Costanzo, P. M. (1984) Synthesis of a 10-Å Hydrated Kaolinite. Clays and Clay Minerals, 32 (1) 29-35 doi:10.1346/ccmn.1984.0320104
Raythatha, Rasik (1985) Mechanism of Synthesis of 10-Å Hydrated Kaolinite. Clays and Clay Minerals, 33 (4) 333-339 doi:10.1346/ccmn.1985.0330409
Battaglia, Stefano, Leoni, Leonardo, Sartori, Franco (2004) The Kübler Index in Late Diagenetic To Low-grade Metamorphic Pelites: A Critical Comparison Of Data From 10 Å and 5 Å Peaks. Clays and Clay Minerals, 52 (1) 85-105 doi:10.1346/ccmn.2004.0520109
Ryan, Peter C., Huertas, F. Javier (2013) Reaction Pathways of Clay Minerals in Tropical Soils: Insights from Kaolinite-smectite Synthesis Experiments. Clays and Clay Minerals, 61 (4) 303-318 doi:10.1346/ccmn.2013.0610410
Fenner, Peter (1969) Laboratory processing of halloysite*. Clays and Clay Minerals, 17 (1) 42-44 doi:10.1346/ccmn.1969.0170110
 
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