JADE
"Jade"
refers to more than one specific type of metamorphic rock. The four
categories of "jade" are:
1) jadeitite (jadeite jade)
2) nephrite/nephritite (nephrite jade)
3) chromian jade (maw sit sit)
4) serpentine jade (not really jade)
Samples
of jadeite jade and kosmochlor jade from Burma are shown below.
Jadeitite (~6.2 cm across along the base) from the Jurassic of Burma. The
light brown-colored rim is a weathering rind. Jadeitite (= jadeite jade)
is a rare metamorphic rock composed of jadeite pyroxene (Na(Al,Fe)(Si2O6)).
Published research on Burmese jade generally indicates that the jadeitite rock
masses formed by metasomatism of albitites (= plagioclase feldspar
metamorphites) at the periphery of serpentinized mantle peridotite
bodies. The mantle peridotite was part of a subducting slab of
Mesozoic-aged oceanic lithosphere that was emplaced upward and against
southeast Asian continental lithosphere by obduction.
Geologic unit: Hpakan-Tawmaw Jade Tract, Hpakan Ultramafic Body, Naga-Adaman
Ophiolite.
Metamorphic age: late Tithonian Stage, near-latest Jurassic, 147 m.y.
Locality:
alluvial clast (placer jade) from unrecorded locality (possibly in the vicinity
of Phakant), upper reaches of the Uyu River (Uru River), western Kachin State,
Indo-Burma Range, northern Burma.
Jadeitite (closeup of above specimen, ~2.2 cm across) from the Hpakan-Tawmaw
Jade Tract (near-latest Jurassic, 147 m.y.) of northern Burma.
Jadeitite (~8.0 cm across at its widest) from the Hpakan-Tawmaw Jade Tract
(near-latest Jurassic, 147 m.y.) of northern Burma. The light
brown-colored rim is a weathering rind. Same geology & age &
general locality as first specimen above.
Kosmochlor jade ("maw sit sit") (8.0 cm across along the
base) from the Hpakan-Tawmaw Jade Tract (near-latest Jurassic, 147 m.y.) of
northern Burma.
Maw sit sit is a very rare, complex, polymineralic
metamorphic rock. Minerals reported in this material include chromite
(metallic black, FeCr2O4), kosmochlor pyroxene
(emerald green to dark green to black, NaCrSi2O6), chromian
jadeite pyroxene (green, Na(Al,Fe,Cr)Si2O6), chromiferous
arfvedsonite amphibole (green or gray, Cr-bearing NaNa2Fe5Si8O22(OH)2),
symplectite (green, a finely-crystalline mineral mix of mostly chromian
jadeite). Reported matrix minerals include thompsonite zeolite, albite
feldspar, or serpentine.
Maw sit sit formed under high pressure and low
temperature conditions at the rim of serpentinized, chromiferous mantle peridotites.
The peridotites were emplaced by obduction as oceanic lithosphere was
subducting beneath the Burmese portion of southeastern Asia during the
Mesozoic.
Geologic unit: northeastern end of the Hpakan-Tawmaw Jade Tract, Hpakan Ultramafic
Body, Naga-Adaman Ophiolite.
Metamorphic age: late Tithonian Stage, near-latest Jurassic, 147 m.y.
Locality:
apparently an alluvial clast derived from the Namshamaw Deposit
("Namshamaw Dike"; "Maw Sit Sit Vein") at Maw Sit Sit, just
northwest of Namshamaw, near Kansi (Kanzi), western Kachin State, Indo-Burma
Range, northern Burma.
Kosmochlor jade ("maw sit sit") (3.15 cm across at its
widest) from the northeastern Hpakan-Tawmaw Jade Tract (near-latest Jurassic,
147 m.y.) of northern Burma. Same geology & age & locality as the
first maw sit sit sample above.
Kosmochlor jade ("maw sit sit") (closeup of above specimen,
1.65 cm across) from the northeastern Hpakan-Tawmaw Jade Tract (near-latest
Jurassic, 147 m.y.) of northern Burma.
Jadeitite (lavender jadeitite) (18.2 cm across at its widest) from the
Hpakan-Tawmaw Jade Tract (near-latest Jurassic, 147 m.y.) of northern
Burma. The light brown-colored rim is a weathering rind. Lavender
is a scarce color variation seen in Burmese jadeitites. Whitish and
near-white jadeite occurs throughout this rock, as well as hints of
pale-greenish gray jadeite near the lower left edge.
Composition: the lavender color of the jadeite clinopyroxene (Na(Al,Fe)(Si2O6))
in this rock appears to be the result of ferrous iron to ferric iron (Fe+2
→ Fe+3) intervalence charge transfer (Rossman, 1974).
Geologic Unit & Age & Locality: Same as the first specimen at top of page.
Jadeitite (lavender jadeitite) (closeup of above specimen, ~7.0 cm across) from
the Hpakan-Tawmaw Jade Tract (near-latest Jurassic, 147 m.y.) of northern
Burma.
Jadeitite (lavender jadeitite) (closeup of above specimen, ~3.8 cm across) from
the Hpakan-Tawmaw Jade Tract (near-latest Jurassic, 147 m.y.) of northern Burma
showing lavender-colored jadeite, whitish to near-whitish jadeite, and hints of
pale-greenish gray jadeite.
Some references on the geology of Burmese jadeitite
and kosmochlor jade:
Rossman, G.R. 1974. Lavender jade, the
optical spectrum of Fe3+ and Fe2+ → Fe3+
intervalence charge transfer in jadeite from Burma. American
Mineralogist 59: 868-870.
Colombo, F., C. Rinaudo & C. Trossarelli.
2000. The mineralogical composition of maw-sit-sit from
Myanmar. Journal of Gemmology 27(2): 87-92.
Shi G.H., Cui W.Y., Wang C.Q. & Zhang W.H.
2000. The fluid inclusions in jadeitite from Pharkant area,
Myanmar. Chinese Science Bulletin 45: 1896-1901.
Kievlenko, E.Y. 2003. Jadeite. pp.
288-302 in Geology of Gems, English Edition. Ocean
Pictures Ltd. Littleton, Colorado.
Shi G.H., B. Stšckhert & Cui W.Y.
2005. Kosmochlor and chromian jadeite aggregates from the Myanmar
jadeitite area. Mineralogical Magazine 69: 1059-1075.
Harlow, G.E., S.S. Sorensen & V.B. Sisson.
2007. Jade. in Geology of gem deposits. Mineralogical
Association of Canada Short Course Series 37: 207-253, pls. 9-1 to 9-7.
Qiu Z.L., Wu F.Y., Yang S.F., Zhu M., Sun J.F. &
Yang P. 2008. Age and genesis of the Myanmar jadeite: constraints
from U-Pb ages and Hf isotopes of zircon inclusions. Chinese Science
Bulletin 54: 658-668.
Shi, G.H., Cui W.Y., Cao S.M., Jiang N., Jian P., Liu
D.Y., Miao L.C. & Chu B.B. 2008. Ion microprobe zircon U-Pb age
and geochemistry of the Myanmar jadeitite. Journal of the Geological
Society of London 165: 221-234.
Shi G.H., Jiang N., Liu Y., Wang X., Zhang Z.Y. &
Xu Y.J. 2009. Zircon Hf isotope signature of the depleted mantle in
the Myanmar jadeitite: implications for Mesozoic intra-oceanic subduction
between the Eastern Indian Plate and Burmese Platelet. Lithos 112:
342-350.
Shi G.H., Wang X., Chu B.B. & Cui W.Y.
2009. Jadeite jade from Myanmar: its texture and gemmological
implications. Journal of Gemmology 31: 185-195.
Shi G.H., Jiang N., Wang Y.W., Zhao X., Wang X., Li
G.W., E. Ng & Cui W.Y. 2010. Ba minerals in clinopyroxene rocks
from the Myanmar jadeitite area: implications for Ba recycling in subduction
zones. European Journal of Mineralogy 22: 199-214.