摘要
黄山东镁铁质-超镁铁质岩体位于东天山北部的土墩-黄山-镜儿泉-图拉尔根镁铁-超镁铁质岩带中段,侵位于元古宙变质岩中。主要岩石类型有二辉橄榄岩、角闪橄榄岩、苏长岩、辉长苏长岩、辉长岩、角闪辉长岩和闪长岩,是一个由3次侵入形成的复式岩体。黄山东岩体单颗粒锆石的176Hf/177Hf值为0.283008～0.283077,平均值为0.283038;176Yb/177Hf值为0.013483～0.050167,平均值为0.031085;176Lu/177Hf值为0.000602～0.002129,平均值为0.001338;εHf(t)(t=274Ma)值为14.20～16.60,平均值为15.20;εHf(0)值为8.30～10.80,平均值为9.40。εNd(t)值为6.6～8.3,初始87Sr/86Sr值为0.7031～0.7038。锆石单颗粒Hf同位素和全岩Sr-Nd同位素组成特征表明,岩体的岩浆源区具有亏损型地幔特征,可能与MORB有关,岩浆在上升过程中只有少量的(小于2%)地壳物质的加入。
The Huangshandong mafic-ultramafic intrusion, is located at the centre segment of Tudun- Huangshan-Jing＂ erquan- Tulaergen mafic-uhramafic rock belt, the northern of the East Tianshan, controlled by the Kangurtag- Huangshan ductile sheer zone, and it is a multiple intrusion formed by at least three pulses of magmas with different compositions, and composes of lherzolite, olivine gabbro, gabbro norite, and gabbro diorite. Sulfide mineralization is associated with the second （gabbronorite） and third （plagioclase-bearing lherzolite-wehrlite） intrusive phases that are volumetrically minor in the intru- sion. The 176 Hf/177 Hf ratios of the Huangshandong zircons range from 0. 283 037 to 0. 283 165 with an average of 0. 283 098; 176Yb/177Hf ratios range from 0. 013 590 to 0. 046 774 with an average of 0. 030 491, that these ratios are all less than 0.05 indicates that little radiogenic Hf has accumulated in these zircons; 176Lu/177Hf ratios range from 0. 000 700 to 0. 002 094 and average 0. 001 318; the eHf（o （t=274 Ma） values range from 15. 38 to 19. 91 and average 17.57; εHf（o） values range from 9.50 to 14. 30 with an average of 11.78. The calculated εNd（t） values and initial ^87 Sr/^86 Sr values （t = 274 Ma） of the Huangshandong intrusive rocks between 6.6 and 8.3, and between 0. 703 1 and 0. 703 8, respectively. The Hf and Sr-Nd isotopic compositions of the Huangshandong intrusion are significantly different from that of the Tarim basahs and coeval mafic-uhramafic dykes in the Tarim basin, similarly with the volcanic arc basahs and consistent with the mid-ocean basahs （MORB）. The results of mixing calculations using Sr-Nd isotopes show that crustal contamination is 〈2% in the Huangshandong parental magmas.
出处
《西北地质》
CAS
CSCD
2012年第4期145-154,共10页
Northwestern Geology
基金
中央高校基本科研业务费专项资金(CHD2011TD007
CHD2012JC004)
西部矿产资源与地质工程教育部重点实验室开放基金(CHD2011SY014)
中国地质调查局地质大调查项目(121201108561)
