|
Lokken, Hoydal, Dragset, Amot |
|
|
Norway |
| Main commodities:
Cu Zn Ag Pb
|
|
The most recent source geological information used to prepare this description was dated: 1989.
Record last updated: 20/11/2012
This description is a summary from published sources, the chief of which are listed below. © Copyright Porter GeoConsultancy Pty Ltd. Unauthorised copying, reproduction, storage or dissemination prohibited.
|
|
|
Grenne T and Slack J F, 2005 - Geochemistry of Jasper Beds from the Ordovician Løkken Ophiolite, Norway: Origin of Proximal and Distal Siliceous Exhalites: in Econ. Geol. v100 pp 1511-1527
|
Grenne T, 1989 - The feeder zone to the Lokken Ophiolite-hosted massive Sulfide deposit and related mineralizations in the central Norwegian Caledonides: in Econ. Geol. v.84 pp. 2173-2195
|
Grenne T, Slack J F 2003 - Bedded jaspers of the Ordovician Lokken ophiolite, Norway: seafloor deposition and diagenetic maturation of hydrothermal plume-derived silica-iron gels: in Mineralium Deposita v38 pp 625-639
|
Grenne T, Vokes F M 1990 - Sea-floor Sulfides at the Hoydal volcanogenic deposit, central Norwegian Caledonides: in Econ. Geol. v85 pp 344-359
|
Grenne, T. and Slack, J.F., 2019 - Mineralogy and geochemistry of silicate, sulfide, and oxide iron formations in Norway: evidence for fluctuating redox states of early Paleozoic marine basins: in Mineralium Deposita v.54, pp. 829-848.
|
|
Porter GeoConsultancy Pty Ltd (PorterGeo) provides access to this database at no charge. It is largely based on scientific papers and reports in the public domain, and was current when the sources consulted were published. While PorterGeo endeavour to ensure the information was accurate at the time of compilation and subsequent updating, PorterGeo, its employees and servants: i). do not warrant, or make any representation regarding the use, or results of the use of the information contained herein as to its correctness, accuracy, currency, or otherwise; and ii). expressly disclaim all liability or responsibility to any person using the information or conclusions contained herein.
|
Top | Search Again | PGC Home | Terms & Conditions
|
|