From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #8335 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 Wednesday, January 19 2022 Volume 14 : Number 8335 Today's Subjects: ----------------- Herpes Virus Hiding Place Revealed! (Nobody Believed This!) ["Cold Sore V] ---------------------------------------------------------------------- Date: Wed, 19 Jan 2022 07:03:34 -0500 From: "Cold Sore Virus" Subject: Herpes Virus Hiding Place Revealed! (Nobody Believed This!) Herpes Virus Hiding Place Revealed! (Nobody Believed This!) http://herpathsy.us/C1b0M1pDVWJi5e4KA7fQaNjuMWiCCRp7SFblZ5XNcD993MpB http://herpathsy.us/G0Fkay8mz5ZkgqJIR8vJruqkhVI6A5acZkqdrQv_sIhb9kY st sedimentary rocks contain either quartz (siliciclastic rocks) or calcite (carbonate rocks). In contrast to igneous and metamorphic rocks, a sedimentary rock usually contains very few different major minerals. However, the origin of the minerals in a sedimentary rock is often more complex than in an igneous rock. Minerals in a sedimentary rock may have been present in the original sediments or may formed by precipitation during diagenesis. In the second case, a mineral precipitate may have grown over an older generation of cement. A complex diagenetic history can be established by optical mineralogy, using a petrographic microscope. Carbonate rocks predominantly consist of carbonate minerals such as calcite, aragonite or dolomite. Both the cement and the clasts (including fossils and ooids) of a carbonate sedimentary rock usually consist of carbonate minerals. The mineralogy of a clastic rock is determined by the material supplied by the source area, the manner of its transport to the place of deposition and the stability of that particular mineral. The resistance of rock-forming minerals to weathering is expressed by the Goldich dissolution series. In this series, quartz is the most stable, followed by feldspar, micas, and finally other less stable minerals that are only present when little weathering has occurred. The amount of weathering depends mainly on the distance to the source area, the local climate and the time it took for the sediment to be transported to the point where it is deposite ------------------------------ End of alt.music.moxy-fruvous digest V14 #8335 **********************************************