Pan-European infrastructure for ocean & marine data management

P01 Vocabulary - Facet Search on Semantic Components

P01 Vocabulary - Facet Search on Semantic Components

The P01 Parameter Usage Vocabulary is based on a semantic model. This model uses a defined set of controlled vocabularies (the semantic components). The Facet Search below facilitates you to search for specific existing P01 terms using components for drilling down.

Are you missing specific P01 terms in the vocabulary, then you can compose and submit new terms for review and uptake using the P01 Vocabulary Builder tool.

Conceptid (87)Preflabel
HMIN0010Proportion of rutile (allothigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0011Proportion of staurolite (allothigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0012Proportion of monazite (allothigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0013Proportion of sphene (allothigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0014Proportion of pyrite (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0015Proportion of siderite (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0016Proportion of haematite (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0017Proportion of galena (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0018Proportion of anatas (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0019Proportion of leucoxene (authigenous) in sediment 50-100um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0020Proportion of ore minerals (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0021Proportion of leucoxene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0022Proportion of amphibole (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0023Proportion of pyroxene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0024Proportion of zircon (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0025Proportion of garnet (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0026Proportion of tourmaline (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0027Proportion of epidote (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0028Proportion of apatite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0029Proportion of rutile (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0030Proportion of staurolite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0031Proportion of monazite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0032Proportion of sphene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0033Proportion of pyrite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy
HMIN0034Proportion of siderite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy