Log in to save to my catalogue

Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechan...

Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechan...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1835594230

Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechanical, and hydrothermal effects: an example from the Nobeoka Thrust, southwest Japan

About this item

Full title

Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechanical, and hydrothermal effects: an example from the Nobeoka Thrust, southwest Japan

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

Journal title

Earth, planets, and space, 2014-12, Vol.66 (1), p.1-12

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

More information

Scope and Contents

Contents

Illite crystallinity (IC), the full width at half maximum of the illite (001) peak in clay-fraction X-ray diffraction (XRD), is a common geothermometer widely applied to various tectonic settings. Paleotemperature estimation using IC presents methodological ambiguity because IC is not only affected by background temperature but also by mechanical,...

Alternative Titles

Full title

Changes in illite crystallinity within an ancient tectonic boundary thrust caused by thermal, mechanical, and hydrothermal effects: an example from the Nobeoka Thrust, southwest Japan

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_1835594230

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1835594230

Other Identifiers

ISSN

1880-5981

E-ISSN

1880-5981

DOI

10.1186/1880-5981-66-116

How to access this item