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  • adj

Synonyms for greenish-grey

of grey tinged with green

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References in periodicals archive ?
Reddened intervals typically have gradational contacts with over-and underlying greenish-grey mudrocks and may contain siderite nodules, carbonized roots, and diffuse organic-rich horizons.
The upper coal occurs above a blocky greenish-grey shale with siderite rhizoconcretions and below a laminated grey shale.
The nodular limestones of the Baltinava Formation are overlain by grey, bedded to nodular, biodetrital limestones with greenish-grey marl interlayers of the Ludza Formation representing the middle part of the Pirgu Stage in the easternmost study area (Ulst 1972; Ulst et al.
In Estonia the lower part of the Adila Formation (Al) is represented by grey to greenish-grey medium- to strongly argillaceous, micro- to very finely crystalline limestones, with a flat to seminodular bedding and discontinuity surfaces in the upper half of the unit.
3: 9) grey variously argillaceous dolostone and dark greenish-grey dolomitized marlstone.
Rare wavy interbeds of greenish-grey dolomitic marlstone occur in the lower part of the member.
Aeronian black shales are overlain by Telychian greenish-grey and red claystones.
The boundary between the Jurmala and Dobele formations is defined as the boundary between black shale and greenish-grey claystone.
The first lithological unit, assigned to the Long Island Member of the Hanford Brook Formation, comprises massive, grey to greenish-grey.
In SE Estonia the sediments of the Zebre Formation are represented by greenish-grey and reddish-brown glauconitic argillaceous dolomite with a thickness up to 4 m.
The argillaceous beds are prevailingly greenish-grey, with very rare small red- or lilac-coloured spots.
The Velise Formation is dominated by grey, bluish-grey, and greenish-grey argillaceous to calcareous, often bioturbated, marlstones, with rare thin interbeds of argillaceous limestone, sometimes rich in bioclastic material.
They come from grey and greenish-grey limestones with thin interlayers of clay containing also ostracodes, bivalves, and scales of thelodonts, fragments of osteostracans and anaspids.