चिकणमाती आणि विलग खडक हा एक ठेव आहे जो त्याच्या मूळ ठिकाणी आढळतो,

saprolite's Usage Examples:

Intensive weathering has created thick zones of saprolite and heavily weathered soils.

arsenic sulfides, and is typically in amorphous to massive infill of lower saprolite ultramafic lithologies.

protolith, saprolitized peridotite, green saprolite (main ore horizon), tachylite (a Fe oxide horizon), black saprolite, yellow and red laterite.

Australian deposits, chrysoprase occurs as veins and nodules with brown goethite and other iron oxides in the magnesite-rich saprolite below an iron and.

5 g/t cutoff value for hard rock and saprolite respectively.

Before it was exposed, groundwater weathered the granite along fracture joints creating corestones of relatively solid altered granite embedded within friable saprolite.

Lavakas form where these hard laterites overlie thick (tens of metres) saprolite, on steep (35 to 55 degree) slopes, in areas that have a hot dry season.

formed in conjunction with saprolite production, the biomantle is the bioturbated zone above the structured (unbioturbated) saprolite, with its base commonly.

various forms of ironstone include siderite nodules; deeply weathered saprolite, i.

"Palaeosurfaces and associated saprolites in southern Sweden".

and Cenozoic, ancient basement rock has weathered into water-bearing saprolite and the region has experienced periods of volcanism and rift valley formation.

by saturating the tailings with water, mining nearby saprolites and clay, sending the saprolites and clay through the ore mills and pouring them over.

Within a European context most of the saprolite mantles of Late Cenozoic age are made up grus, contrasting with Mesozoic and Early.

Synonyms:

earth, ground,

Antonyms:

disconnect, unfasten, figure,