Recognizing illitization progress from diagenesis to very low-grade metamorphism in rocks of the Cantabrian Zone (Spain)

Schweizerische Mineralogische und Petrographische Mitteilungen

Volumn 82, Issue 2, 2002, Pages 211-219

  Brime, Covadonga ^a   Castro, Marcos ^a   Valín, Ma Luz ^a  

^a UNIVERSITY OF OVIEDO   (Spain)

Author keywords

Crystallite thickness distributions (CTDs); Decomposition; Illite; X ray diffraction

Indexed keywords

DIAGENESIS; ILLITIZATION; LOW GRADE METAMORPHISM; PALEOZOIC; X-RAY DIFFRACTION;

SPAIN;

EID: 0036377768     PISSN: 00367699     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (47)

1. The status of clay mineral structures
2. Tectono-thermal evolution in a region with thin skinned tectonics: The western nappes in the Cantabrian Zone (Variscan belt of NW Spain)
3. Tectono-thermal evolution of the Cantabrian Zone (NW Spain)
4. Definition of low grade metamorphic zones using illite crystallinity
5. Postdepositional transformation of clays in Palaeozoic rocks of northwest Spain
6. A diagenesis to metamorphism transition in the Hercynian of NW Spain
7. Growth mechanism of low grade illites based on shape of crystal growth distributions
8. Transition from diagenesis to metamorphism near the front of the Variscan Regional Metamorphism (Cantabrian Zone, Northwestern Spain)
9. La transición diagénesis-metamorfismo en la región de Cabo Peñas
10. XRD measurement of mean thickness, thickness distribution and strain for illite and illite-smectite crystallites by the Bertaut-Warren-Averbach technique
11. Ostwald ripening of clays and metamorphic grade
12. Deducing growth mechanisms for minerals from the shape of crystal size distributions
13. MudMaster: A program for calculating crystallite size distributions and strain from the shapes of X-ray diffraction peaks
14. Measurement of fundamental illite particle thickness by X ray diffraction using PVP-10 intercalation
15. Simultaneous use of thermal indicators to analyse the transition from diagenesis to metamorphism: An example from the Variscan Belt of northwest Spain
16. The transformation of illite to muscovite in pelitic rocks: Constrains from X-ray diffraction
17. Illite polytype quantifications and K/ Ar dating of Paleozoic shales: A technique to quantify diagenetic and detrital illite
18. Profile fitting of powder difraction patterns
19. Illite "crystallinity" revisited
20. Transmission and analytical electron microscopic study of mixed layer illite/smectite formed as a replacement product of diagenetic illite
21. Crystal growth mechanisms in miarolitic cavities in the Lake George ring complex and vicinity, Colorado
22. An assessment of calcite crystal growth mechanisms based on crystal growth distributions
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26. Application de la décomposition des diffractogrammes de rayons-X à l'identification des minéraux argileux
27. Characterization of the end of smectite-to-illite transformation: Decomposition of X ray patterns
28. The I/S-to-illite reaction in the late stage diagenesis
29. Decomposition of X-ray diffraction patterns: A convenient way to describe complex I/S diagenetic evolution
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31. Evolution de la structure cristallographique des minéraux argileux dans le réservoir gréseux Rotliegend des Pays-Bas
32. Low grade metamorphism in the Scottish Southern Uplands terrane: Deciphering the patterns of accretionary burial, shearing and cryptic aureoles
33. Diagenesis of the Purington Shale in the Illinois basin and implications for the diagenetic state of sedimentary rocks of shallow Paleozoic basins
34. A comparative XRD and TEM study of the physical meaning of the white mica 'crystallinity' index
35. Diagenesis and low grade metamorphism of shales and slates
36. Mineralogical and morphological evidence for the formation of illite at the expense of illite/smectite
37. Mafic phyllosilicates in low-grade metabasites. Characterization using deconvolution analysis
38. Profile fitting for quantitative analysis in X ray powder diffraction
39. Evolution of fundamental particle size during illitization of smectite and implications for the illitization mechanism
40. Deconvolution of the first 'illite' basal reflection
41. Deconvolution of the X-ray 'Illite' 10-A complex: A case study of the Helvetic sediments from eastern Switzerland