Nephrite Jade from Guangxi Province, China
Nephrite jade with high market value and production potential from the Chinese city of Hechi, in Guangxi Province, was tested by standard gemological methods, polarizing microscopy, scanning electron microscopy (SEM), X-ray diffraction (XRD), Raman spectroscopy, and energy-dispersive spectrometry (EDS). The three samples were mainly white and gray-white (with areas of gray, gray-green, dark green, and black) and had a greasy to waxy luster. Within each of these color varieties, the samples exhibited either “band” or dendritic patterns. The band pattern, composed of tremolite, varied in shape and was either transparent or opaque. Its color, transparency, and distribution were different from the unpatterned areas. The dendritic patterns, which had a brownish yellow and dark brown to black color, were composed of chlorite that formed during metamorphism.
Nephrite is favored by Chinese collectors for its color and luster, as well as its fine texture and outstanding toughness. Primary nephrite deposits are found in more than 20 countries, including China, Russia, Canada, Australia, New Zealand, and South Korea. Chinese deposits are mainly distributed in the areas of Xinjiang, Qinghai, Guizhou, and Liaoning (Liao et al., 2005; Zhang et al., 2011). Research shows that nephrite’s excellent toughness is a product of its fine-grained interlocking structure (Bradt et al., 1973; Dorling and Zussman, 1985; Yang, 2011). Its green color is due mainly to the substitution of Cr3+ and Fe2+ for Mg2+ (Flint, 1990). In principle, nephrite can form in two different ways. One is by contact metasomatism between intermediate-acidic intrusive rocks and dolomite and/or limestone. The other is by contact metasomatism between serpentine or serpentinizing peridotite and more silicic rocks (Harlow and Sorensen, 2005; Siqin et al., 2012).
The Chinese nephrite samples in this study were recovered in 2012 from Dahua County, in the city of Hechi. There are several mines in the county, worked by independent miners who also farm the area. One farmer estimated production of more than 1,000 tons per year. The local government controls the mining, and the market for this nephrite is growing in Guangxi and Guangdong. In 2013, the pendant shown in figure 1 sold for US$300, while the bangles in figure 5 brought US$3,000 each.
This paper introduces the mine at Hechi and characterizes the patterns in these nephrites.
GEOLOGIC BACKGROUND AND LOCATIONThe nephrite mining area at Hechi, shown in figure 2, belongs to the west wing of the NNE-striking (15°–30°) Yangshan-Damingshan anticline. Regional strata dip steeply, and almost all main structural features strike NNE. The wall rocks are marine carbonate rocks deposited from the Upper Devonian to Lower Permian periods (362–290 Ma). Basic intrusive and volcanic rocks were emplaced during the Permian period (approximately 295–250 Ma). The heat generated by the emplacement caused metasomatism between the igneous rocks and the carbonate rocks. Nephrite is the product of this metasomatism (Bureau of Geology and Mineral Resources of Guangxi Province, 1985).
The mining area has a typical karst landscape. It has been severely weathered by the subtropical climate, and slope sediments, fluvial, and alluvial materials are all visible. The ore-bearing country rocks are limestone, in severely weathered layers of varying thickness. Nephrite occurs as bands and veins in these layers. The width of a single vein ranges from tens of centimeters to several meters. The ore body and wall rock (mainly dolomite marble) are alternately distributed, and the boundary between them is sharp.
The nephrites from these primary and secondary mines are mainly white, gray-white, gray-green, dark green, and black, with a greasy to waxy luster (figure 3). All of these color varieties display either band or dendritic patterns. The band patterns are white and opaque, and their color, transparency, and distribution are different from those of the unpatterned areas. The dendritic patterns are brownish yellow and dark brown to black (figure 4). At Hechi, the dendritic patterns only occur in the nephrites from secondary deposits in river or soil.
MATERIALS AND METHODSThree white and gray-white nephrite samples were examined for this study: the two bangles with dendritic patterns (figure 5, left and center) and a slab with a band pattern (figure 5, right). The dendritic patterns in the two bangles ranged from brownish yellow to black. In the slab, the banded area showed lower transparency than the rest of the sample. The samples were tested by standard gemological methods, polarizing microscopy, scanning electron microscopy (SEM), X-ray diffraction (XRD), Raman spectroscopy, and energy-dispersive spectrometry (EDS). We conducted the tests at the National Key Lab of the China University of Geosciences in Wuhan.
For SEM analysis, the authors fractured the specimens and coated the fracture surfaces with carbon powders using an SCD-005 ion sputter coater. The specimens were then fastened to a round metal disk for observation. An FEI Quanta 200 scanning electron microscope was used to observe the nephrites’ microstructure, especially their dendritic and band patterns. The SEM images are from secondary electrons.
The instrument used for XRD analysis was an X’Pert PRO DY 2198 with Cu Kα radiation operating at 40 kV and 40 mA. The instrument was equipped with a small platform and a monocapillary lens with a 100 μm diameter micro-zone. Dendritic patterns were tested by the micro-area method, since it is difficult to detect very small particles through normal analysis.
To detect the mineral composition of the patterns, we used a Bruker Senterra scanning Raman microscope in the 40–3650 cm–1 region. The instrument, which features a 785 nm light source and 50 mW laser energy, was set to approximately 3.5 cm–1 resolution and 10 seconds per scan. Dendritic, band, and unpatterned areas were all tested.
For EDS analysis of the dendritic and band patterns, we used an EDAX Genesis 2000. This element-testing method employs back-scattered electrons to obtain chemical composition. Measurement error with the EDS data is 0.1–0.5%.
RESULTS AND DISCUSSIONGemological Features and Petrographic Study. The samples showed a spot RI of 1.61–1.62 and a hydrostatic SG of 2.88–2.90. The unpatterned and band areas of the nephrite slab were sliced into thin sections. Under polarized light, they displayed different microstructures. The tremolites of the band area (figure 6, left) were fibrous, columnar, of various grain size, and poorly oriented. The individual tremolite crystals ranged from less than 0.05 to 0.2 mm long, occurring in radial beam and fan shapes. The band had a coarser texture than the unpatterned area. The interwoven tremolites of the unpatterned area (figure 6, right) were fine, with a homogeneous grain size. Most of the tremolites were less than 0.05 mm long.
SEM. We performed SEM testing of the dendritic areas in the two bangles, and the band and unpatterned areas of the slab. The tremolites with a dendritic pattern were magnified 1514× and 2840× (figure 7). The tremolite grains occurred as long strips, the dendritic pattern grains as tiny dots. At 2840× magnification, the tremolite grains were clearly visible, while the grain shape of the dendritic pattern was not.
The grains in the band areas were unevenly distributed, while those in the unpatterned areas were uniformly distributed at 500× magnification. At 2000× magnification, the grains in the band were poorly oriented, while those in the unpatterned areas were better oriented (figure 8). Those distinctions led to different appearances between these two areas of the sample.
Raman Spectroscopy. The grains of the dendritic patterns were too small to detect by Raman, even though the dendritic patterns themselves appeared quite large. Only the spectra of the band and unpatterned areas are provided.
According to the Raman spectra of the slab (figure 9), the mineral constituents of the band and unpatterned portions were all tremolites. Among the nephrite peaks, the 3600–3700 cm–1 features represent O-H stretching vibration, and the 900–1150 cm–1 features represent the stretching vibration and antisymmetric stretching vibration of the Si-O bond. The 677 cm–1 band designates the symmetric stretching vibration of Si-O-Si. The 100–400 cm–1 features may be caused by the deformation vibration induced by the distortion vibration of the silicon oxygen tetrahedron (Zhao and Gan, 2009; Qiu et al., 2010; Yang et al., 2012).
To verify the dendritic patterns by means of their crystal structure and chemical composition, we turned to XRD and EDS.
XRD. To identify the mineral crystal structure of the dendritic pattern, we used the micro-area XRD method, the results of which are shown in figure 10. According to Bragg’s law, defined as
“d” is the crystal lattice spacing in a certain direction. The dendritic pattern gave d values of 14.4, 7.1, 4.7, 3.5, and 2.8 Å, confirming that the mineral belonged to the chlorite group (Bailey and Lister, 1989; Zhao et al., 2006).
Chemical Composition. The dendritic, band, and unpatterned areas were all tested by EDS. The main composition of the dendritic pattern (table 1) was consistent with chlorite, which has a general chemical formula of Y3[Z4O10](OH)2•Y3(OH)6, where Y can represent Ca, Mg, Fe2+, Al, Fe3+, Cr, Ni, Mn, V, Cu, or Li, and Z is mainly Si and Al. According to table 1, the formula of chlorite here is (Ca, Mg, Mn, Fe)[Si4O10](OH)2(Ca, Mg, Mn, Fe)(OH)6. The band (table 2) and unpatterned areas (table 3) were both consistent with tremolite.
Tables 1-3 (PDF)