CORE
🇺🇦
make metadata, not war
Services
Services overview
Explore all CORE services
Access to raw data
API
Dataset
FastSync
Content discovery
Recommender
Discovery
OAI identifiers
OAI Resolver
Managing content
Dashboard
Bespoke contracts
Consultancy services
Support us
Support us
Membership
Sponsorship
Community governance
Advisory Board
Board of supporters
Research network
About
About us
Our mission
Team
Blog
FAQs
Contact us
Low-temperature smectite illitization as a biomineral process
Authors
Khramchenkov M.
Krinari G.
Publication date
1 March 2020
Publisher
Abstract
This paper studies the low-temperature illitization of smectite in arid basins, where fresh sediments underwent drastic changes in redox potential. We examined Upper Permian sediments from Tatarstan and the Komi Republic, as well as Lower Triassic and Upper Jurassic sediments from the Moscow syneclise (the upper Volga region. The data obtained indicate that smectite illitization can involve at least two different mechanisms, one of which is related to biota activity and does not require temperature increase. The later dissolution-reprecipitation involves both semectite and secondary mica sheets, which affect both the kinetics of the reaction and the structure of its products. Copyright © 2005 by Pleiades Publishing, Inc
Similar works
Full text
Available Versions
National Open Repository Aggregator (NORA)
See this paper in CORE
Go to the repository landing page
Download from data provider
oai:rour.neicon.ru:rour/173374
Last time updated on 04/04/2020