Controls on the formation of a large Zn-Pb Irish-type deposit: evidence from the Navan halos

Author(s)
Uri
Date Issued
2017-05-14
Date Available
2018-05-08T15:18:44Z
Abstract
The mainly epigenetic Navan orebody is hosted by the Lower Carboniferous shallow water carbonate Pale Beds. Subordinate mineralization, hosted by submarine debris flows and the lowermost overlying basinal rocks, formed during seafloor exhalation and reaches ore grade in the Conglomerate Group Ore.
Type of Material
Conference Publication
Publisher
Irish Association for Economic Geology
Subjects

Orebodies

Navan

Web versions
Language
English
Status of Item
Not peer reviewed
Conference Details
IAEG Annual Conference 2017, Sligo, Ireland, 12-14 May 2017
This item is made available under a Creative Commons License
File(s)
Loading...
Thumbnail Image
Name

50_Marks_et_al_17_IAEG_Navan.pdf

Size

162.12 KB

Format

Adobe PDF

Checksum (MD5)

fc6c8ec67f6e4d0ff718c7d21e62575d

Owning collection
Earth Sciences Research Collection
Mapped collections
ICRAG Research Collection