Citation: | WU Lei,ZHAI Xinwei,WANG Erteng,et al. Geochemical Characteristics and Tectonic Setting of the Jijitaizi Ophiolite in Beishan area[J]. Northwestern Geology,2025,58(1):27−42. doi: 10.12401/j.nwg.2023038 |
The Jijitaizi ophiolite belt in the middle of the Beishan orogenic belt, between the Mingshui-Hanshan microcontinental block and the Gongpoquan unit is an important part of the Jijitaizi-Xiaohuangshan ophiolite belt, composed of ultrabasic rocks, gabbro and basalt. To reveal the tectonic setting of Jijitaizi ophiolite belt, gabbro and basalt are selected for petrological and geochemical studies. MgO of gabbro and basalt is 6.04%~6.73% and 6.21%~9.66%, Mg# values are 32.33~37.03, 27.58~46.27, respectively, SI consolidation index is 27.66~31.55 and 24.96~42.20, Al2O3 is 15.82%~16.79% and 13.38%~15.38%, Na2O higher than K2O content (Na2O/K2O=9.75~17.15, 1.95~23.26), Na2O+K2O is 4.48%~4.90% and 3.3%~4.68%, P2O5 is 0.07%~0.09% and 0.16%~0.27%. Both of gabbro and basalt enrichment of LILEs and LREE, depletion of HREE and HFSEs and Eu have no obvious anomalies (δEu=0.98~1.09、0.88~1.06). (87Sr/86Sr)i is
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