Mixed-layer mica-chlorite in very low-grade metaclastites from the Malaguide Complex (Betic Cordilleras, Spain)

Author: Cruz M.D.R.

Source: Clay Minerals, Volume 36, Number 3, 1 September 2001 , pp. 307-324(18)

Publisher: Mineralogical Society

Buy & download fulltext article:

OR

Price: $14.18 plus tax (Refund Policy)

Abstract:

Mixed-layered phyllosilicates with composition intermediate between mica and chlorite were identified in very low-grade metaclastites from the Maláguide Complex (Betic Cordilleras, Spain), and studied by X-ray diffraction, and transmission and analytical electron microscopy. They occur both as small grains in the rock matrix, and associated with muscovitechlorite stacks. Transmission electron microscope observations revealed a transition from chlorite to ordered 1:1 interstratifications through complex 1:2 and 1:3 interstratifications. Analytical electron microscopy data indicate a composition slightly different from the sum of discrete trioctahedral chlorite and dioctahedral mica. The types of layer transitions suggest that mixed-layer formation included two main processes: (1) the replacement of a brucite sheet by a cation sheet in the chlorite structure; and (2) the precipitation of mica-like layers between the chlorite layers. The strongest diffraction lines in oriented X-ray patterns are: 12.60 Å (002), 7.98 Å (003), 4.82 Å (005) and 3.48 Å (007).

Keywords: ALPINE; METAMORPHISM; BETIC; CORDILLERAS; BIOTITE; CHLORITE; MIXED; LAYER; MUSCOVITE; TEM/AEM

Language: English

Document Type: Research article

Publication date: 2001-09-01

More about this publication?
Related content

Tools

Key

Free Content
Free content
New Content
New content
Open Access Content
Open access content
Subscribed Content
Subscribed content
Free Trial Content
Free trial content

Text size:

A | A | A | A
Share this item with others: These icons link to social bookmarking sites where readers can share and discover new web pages. print icon Print this page