Jump to content

User talk:F.guzzo.1

Page contents not supported in other languages.
From Wikipedia, the free encyclopedia

F.guzzo.1, you are invited to the Teahouse!

[edit]
Teahouse logo

Hi F.guzzo.1! Thanks for contributing to Wikipedia.
Be our guest at the Teahouse! The Teahouse is a friendly space where new editors can ask questions about contributing to Wikipedia and get help from experienced editors like Lectonar (talk).

We hope to see you there!

Delivered by HostBot on behalf of the Teahouse hosts

16:05, 20 November 2018 (UTC)

comments on automicrite

[edit]

Ciao F., there are a couple of things you should work on in your text. One is, you should give, or refer to, a definition of mud mounds for the casual reader, otherwise the part of txt about automicrite-made platforms is only understandable by insiders. A second is, your short chapter "features" appears to describe micrite or carbonate mud, not automicrite. In particular, it is not correct to state that "its analogue in siliciclastic sediment is shale". A shale was transported and deposited, automicrite is authigenic, and has never been transported and deposited. --Nereo Preto (talk) 14:46, 15 January 2019 (UTC)[reply]