Mirah kuning: Perbedaan antara revisi

|gravity = 3.27–4.5<ref name="Smith1999">{{cite book|author=Mick R. Smith|title=Stone: Building Stone, Rock Fill and Armourstone in Construction|url=http://books.google.com/books?id=Xcuoyxo33nsC&pg=PA62|year=1999|publisher=Geological Society of London|isbn=978-1-86239-029-4|pages=62–|quote=Specific Gravity 3.5-4.5}}</ref><ref name="Kogel2006">{{cite book|author=Jessica Elzea Kogel|title=Industrial Minerals & Rocks: Commodities, Markets, and Uses|url=http://books.google.com/books?id=zNicdkuulE4C&pg=PA679|year=2006|publisher=SME|isbn=978-0-87335-233-8|pages=679–|quote=The specific gravity is approximately 3.2 when pure rises with increasing iron content.}}</ref><ref>{{cite web|url=http://www.science.smith.edu/geosciences/petrology/Petrography/Olivine/Olivine.html |title=Olivine |publisher=Science.smith.edu |date= |accessdate=2013-11-14 |quote=G = 3.22 to 4.39. Specific gravity increases and hardness decreases with increasing Fe.}}</ref><ref>{{cite web|url=http://www.geo.umn.edu/courses/1001/minerals/olivine.shtml |title=University of Minnesota’s Mineral Pages: Olivine |publisher=Geo.umn.edu |date= |accessdate=2013-11-14 |quote=Specific Gravity: 3.2 (Mg-rich variety) to 4.3 (Iron-rich variety) (average weight)}}</ref>

|last = Klein

|first = Cornelis

|coauthors = and C. S. Hurlburt

|title = Manual of Mineralogy |edition=21st

|publisher = John Wiley & Sons

|year = 1985

|location = New York

|isbn = 0-471-80580-7}}</ref>