From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #15161 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Thursday, December 5 2024 Volume 14 : Number 15161 Today's Subjects: ----------------- Say Goodbye to Mess! ["Special Offer" ] ---------------------------------------------------------------------- Date: Thu, 5 Dec 2024 13:56:38 +0100 From: "Special Offer" Subject: Say Goodbye to Mess! Say Goodbye to Mess! http://simplejointpain.click/ct51eyqqZepczItiGdz7N-zNp0SfHsvQUT0ygAKVYX9b4ossOg http://simplejointpain.click/Fsigawx4PDJqneLf_jjml5GHaj2niPrSu-gI3YutiFW9PP3Tkg eletal fragments of marine organisms such as coral or foraminifera. These organisms secrete structures made of aragonite or calcite, and leave these structures behind when they die. Other carbonate grains composing limestones are ooids, peloids, and limeclasts (intraclasts and extraclasts ). Skeletal grains have a composition reflecting the organisms that produced them and the environment in which they were produced. Low-magnesium calcite skeletal grains are typical of articulate brachiopods, planktonic (free-floating) foraminifera, and coccoliths. High-magnesium calcite skeletal grains are typical of benthic (bottom-dwelling) foraminifera, echinoderms, and coralline algae. Aragonite skeletal grains are typical of molluscs, calcareous green algae, stromatoporoids, corals, and tube worms. The skeletal grains also reflect specific geological periods and environments. For example, coral grains are more common in high-energy environments (characterized by strong currents and turbulence) while bryozoan grains are more common in low-energy environments (characterized by quiet water). Ooids (sometimes called ooliths) are sand-sized grains (less than 2mm in diameter) consisting of one or more layers of calcite or aragonite around a central quartz grain or carbonate mineral fragment. These likely form by direct precipitation of calcium carbonate onto the ooid. Pisoliths are similar to ooids, but they are larger than 2 mm in diameter and tend to be more irregular in shape. Limestone composed mostly of ooids is call ------------------------------ End of alt.music.moxy-fruvous digest V14 #15161 ***********************************************