- https://data.geoscience.earth/ncl
- INSPIRE
- MineralDepositGroupValue
- _5b10a056-21db-4a59-85e3-d3d90376d486
experimental
Entry: sediment-hosted
URI: http://inspire.ec.europa.eu/codelist/MineralDepositGroupValue/sedimentHosted
Sediment-hosted deposits can be divided into two major subtypes. The first subtype is clastic-dominated lead-zinc ores, which are hosted in shale, sandstone, siltstone, or mixed clastic rocks, or occur as carbonate replacement, within a clastic-dominated sedimentary rock sequence. This subtype includes deposits that have been traditionally referred to as sedimentary exhalative (SEDEX) deposits. The second subtype of sediment-hosted Pb-Zn deposits is the Mississippi Valley-type that occurs in platform carbonate sequences, typically in passive-margin tectonic settings.
Core metadata
| is a | Concept |
| submitted by | Sophie Chaduteau |
| accepted on | 16 Jul 2026 11:52:37.285 |
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All metadata properties
| date accepted |
16 Jul 2026 11:52:37.285
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| date submitted |
16 Jul 2026 09:20:11.014
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| definition |
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| item class |
Concept
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| label |
sediment-hosted
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| notation |
5b10a056-21db-4a59-85e3-d3d90376d486
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| register |
mineral deposit group value
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| status |
status experimental
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| type |
register item
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| version info |
2
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Definition
| definition |
Sediment-hosted deposits can be divided into two major subtypes. The first subtype is clastic-dominated lead-zinc ores, which are hosted in shale, sandstone, siltstone, or mixed clastic rocks, or occur as carbonate replacement, within a clastic-dominated sedimentary rock sequence. This subtype includes deposits that have been traditionally referred to as sedimentary exhalative (SEDEX) deposits. The second subtype of sediment-hosted Pb-Zn deposits is the Mississippi Valley-type that occurs in platform carbonate sequences, typically in passive-margin tectonic settings.
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| in scheme |
Mineral Deposit Group Value
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| notation |
sedimentHosted
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| pref label |
sediment-hosted
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| type |
Concept
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