# Concept

## sediment 140-250um [heavy fraction phase]

URI | http://vocab.nerc.ac.uk/collection/S26/current/MAT00962/1/ | |
---|---|---|

Within Vocab | BODC parameter semantic model matrices | |

Alternative Labels | ||

Definition | Disaggregated minerals or mineraloids that sink in bromoform (density 2.89g/cm3) from a sample collected on a 140um sieve after passing through a 250um sieve. | |

Date | 2014-06-03T12:16:35 | |

Identifier | SDN:S26::MAT00962 | |

Note | accepted | |

Is Version Of | MAT00962 | |

version | 1 | |

Broader | `S21:S21S022` | sediment |

`S01:S018` | matrix entity | |

Narrower | `P01:HMIN0064` | Proportion of kyanite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy |

`P01:HMIN0023` | Proportion of pyroxene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0027` | Proportion of epidote (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0061` | Proportion of brookite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0029` | Proportion of rutile (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0022` | Proportion of amphibole (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0026` | Proportion of tourmaline (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0024` | Proportion of zircon (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0030` | Proportion of staurolite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0028` | Proportion of apatite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0037` | Proportion of anatas (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0032` | Proportion of sphene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0031` | Proportion of monazite (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0058` | Proportion of barite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0021` | Proportion of leucoxene (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0025` | Proportion of garnet (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0034` | Proportion of siderite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0038` | Proportion of leucoxene (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0036` | Proportion of galena (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0020` | Proportion of ore minerals (allothigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0033` | Proportion of pyrite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

`P01:HMIN0035` | Proportion of haematite (authigenous) in sediment 140-250um [heavy fraction phase] by separation in bromoform and optical microscopy | |

Related | `S23:S23C011` | heavy fraction |

`S22:S22C0047` | 140-250um |

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