The complexity of mudstone diagenesis–some insight from the Tøyen Shale, Lower to Middle Ordovician, southern Sweden

Research output: Contribution to journalArticle

Abstract

The Lower to Middle Ordovician Tøyen Shale in southern Sweden, a biostratigraphically well-dated siliciclastic mudstone unit, shows 18 distinct authigenic cements that include sulfides, carbonates, silicates, clays, and phosphates. Marcasite, sphalerite, galena, and six texturally distinct types of pyrite characterize the sulfides whereas only one type of dolomite and three different generations of calcite are observed in this unit. Quartz, phosphate, and organic matter occur as only one generation each. Authigenic clay minerals are represented by chlorite and kaolinite. The paragenetic sequence of cements is subdivided into the two pre-burial carbonates, succeeded by ten relatively early burial cements, and six late burial cements, the kaolinite being the latest of them all and potentially being of Cretaceous age. Based on textural relationships, the paragenetic sequence of alterations started with dolomite precipitation followed by calcite, and then five different generations of pyrite. All eleven other phases post-date these initial seven cements in the Tøyen Shale.

Details

Authors
  • Sven O. Egenhoff
  • Neil S. Fishman
  • Heather A. Lowers
  • Per Ahlberg
Organisations
External organisations
  • Colorado State University
  • Petrologic Solutions LLC
  • United States Geological Survey, Reston
Research areas and keywords

Subject classification (UKÄ) – MANDATORY

  • Geology

Keywords

  • dolomite formation, Lower to Middle Ordovician, Shale diagenesis, Tøyen Formation
Original languageEnglish
Pages (from-to)54-67
JournalGFF
Volume141
Issue number1
Early online date2018 Nov 9
Publication statusPublished - 2019
Publication categoryResearch
Peer-reviewedYes