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- W2150838412 abstract "SUMMARYPetrographic examination of some Werfenian limestones of the Dolomite region in northeastern Italy has revealed these iimestones to show an unusual granular texture. This texture seems to have originated during an early resedimentation attempt when the sediments in which they occur were still water impregnated. Because these “pseudo-grains” never existed as free clastic entities but yet recall intraclastic grains they are defined as protointruclusts and the rock as protointruclastic micrite." @default.
- W2150838412 created "2016-06-24" @default.
- W2150838412 creator A5090906288 @default.
- W2150838412 date "1966-07-01" @default.
- W2150838412 modified "2023-09-24" @default.
- W2150838412 title "PROTOINTRACLASTS: TEXTURE OF SOME WERFENIAN (LOWER TRIASSIC) LIMESTONES OF THE DOLOMITES (NORTHEASTERN ITALY)" @default.
- W2150838412 cites W1872967972 @default.
- W2150838412 doi "https://doi.org/10.1111/j.1365-3091.1966.tb01899.x" @default.
- W2150838412 hasPublicationYear "1966" @default.
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