lcags rdo: Difference between revisions

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'''lcags kyi rdo ba'''s tshe 'phel bcud len byed / ces par ka dog nag po dang ser po gnyis / gang yang lci la bzhus na lcags 'byungs ba de yin / rgyu ngar mnyen gnyis pho mo rgod g.yung rim pa'o // (Shel gong shel phreng, pdf p 115.1) <br>
'''lcags kyi rdo ba'''s tshe 'phel bcud len byed / ces par ka dog nag po dang ser po gnyis / gang yang lci la bzhus na lcags 'byungs ba de yin / rgyu ngar mnyen gnyis pho mo rgod g.yung rim pa'o // (Shel gong shel phreng, pdf p 115.1) <br>


The chief ores of iron consist mainly of the oxides: hematite ('''[[mdung rtse smug po]]'''), goethite ('''[[mdung rtse dkar po]]''') or limonite ('''[[sin dhu ra]]'''); and the carbonate siderite. Siderite, FeCO<sub>3</sub>, can be yellowish- to greyish-brown, green, red and black. Fungi like ''Lichenothelia'' may oxidize iron to produce siderite, which is then a biomineral. Often found in bedded sedimentary deposits with a biological component, suggesting a biogenical origin. Numerous sites in Tibet. (mindat. org) <br>
Several names and notices in the Shel phreng deal with iron oxides, commonly identified as Limonite : '''[[lcags rdo]]''' in the meltable medicinal stone section, '''[[gru bzhi]]''' and '''[[btsag]]''' as well as '''[[smug po sbal rgyab]]''' and '''[[smug po chig thub]]''' within the non-meltable medicinal stones, and '''[[sin dhu ra]]''' in the medicinal earth section. <br>
The chief ores of iron consist mainly of the oxides, like Hematite, Goethite  or Limonite ; as well as the carbonate Siderite. Siderite (FeCO<sub>3</sub>) can be yellowish- to greyish-brown, green, red and black. Fungi like ''Lichenothelia'' may oxidize iron to produce Siderite, which is then considered a biomineral. Often found in bedded sedimentary deposits with a biological component, suggesting a biogenical origin. Numerous sites in Tibet. (mindat. org) <br>
[[User:Johannes Schmidt|Johannes Schmidt]] ([[User talk:Johannes Schmidt|talk]]) 06:35, 25 February 2024 (EST)
[[User:Johannes Schmidt|Johannes Schmidt]] ([[User talk:Johannes Schmidt|talk]]) 06:35, 25 February 2024 (EST)


  [[Category:Tibetan Dictionary]] [[Category:rydic2003]] [[Category:ca]]
  [[Category:Tibetan Dictionary]] [[Category:rydic2003]] [[Category:ca]]

Revision as of 07:58, 21 May 2024

This is the RYI Dictionary content as presented on the site http://rywiki.tsadra.org/, which is being changed fundamentally and will become hard to use within the GoldenDict application. If you are using GoldenDict, please either download and import the rydic2003 file from DigitalTibetan (WayBack Machine version as the site was shut down in November 2021).

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ལྕགས་རྡོ

shotput, flint stones, iron stone, iron ore [JV]

iron ore [RY]


(med) Iron ore (Drungtso 1999), Limonite (Yeshi 2018)
Synonyms : gru bzhi, brgya rdo, zhang blon bla rdo, sin dhu ra, rgya mtsho'i breg pa, mkha 'gro'i mnyal khrag (Yeshi 2018).

lcags kyi rdo bas tshe 'phel bcud len byed / ces par ka dog nag po dang ser po gnyis / gang yang lci la bzhus na lcags 'byungs ba de yin / rgyu ngar mnyen gnyis pho mo rgod g.yung rim pa'o // (Shel gong shel phreng, pdf p 115.1)

Several names and notices in the Shel phreng deal with iron oxides, commonly identified as Limonite : lcags rdo in the meltable medicinal stone section, gru bzhi and btsag as well as smug po sbal rgyab and smug po chig thub within the non-meltable medicinal stones, and sin dhu ra in the medicinal earth section.
The chief ores of iron consist mainly of the oxides, like Hematite, Goethite or Limonite ; as well as the carbonate Siderite. Siderite (FeCO3) can be yellowish- to greyish-brown, green, red and black. Fungi like Lichenothelia may oxidize iron to produce Siderite, which is then considered a biomineral. Often found in bedded sedimentary deposits with a biological component, suggesting a biogenical origin. Numerous sites in Tibet. (mindat. org)
Johannes Schmidt (talk) 06:35, 25 February 2024 (EST)