西准噶尔哈拉阿拉特山一带晚石炭世赞岐岩的发现及其地质意义
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摘要
西准噶尔哈拉阿拉特山一带广泛分布晚石炭世玄武安山岩、辉石安山岩,属钙碱性系列,岩石具有较高的SiO_2(52.88%~56.89%)、MgO(3.47%~6.88%,Mg#为48.5~63.7)、Sr(442×10~(-6)~970×10~(-6))、Ba(199×10~(-6)~796×10~(-6))含量,K/Na为0.22~0.70,P_2O_5变化范围较大(0.18%~0.52%),富集大离子亲石元素和轻稀土元素((La/Yb)N为1.88~15.9),亏损Nb、Ta、Hf等高场强元素和重稀土元素,弱负Eu异常(δEu=0.77~0.94),(87Sr/86Sr)i=0.70366~0.70409,(~(143)Nd/~(144)Nd)i=0.51247~0.512564,εNd(t)=4.41~6.19,~(206)Pb/~(204)Pb=18.220~18.405,~(207)Pb/~(204)Pb=15.482~15.522,~(208)Pb/~(204)Pb=37.991~38.296,与典型赞岐岩地球化学特征一致。该赞岐岩的厘定,为研究西准噶尔构造演化提供了新的思路,约束了本区残余洋盆的闭合时限并非前人确立的早石炭世,而应延迟至晚石炭世末期。
The Late Carboniferous volcanic rocks consist of basaltic andesite and pyroxene andesite which are widespread in Hala'alate Mountain,West Junggar. The volcanic rocks belong to calc-alkaline series and show a remarkable geochemical affinity with Cenozoic sanukitoids of the Setouchi Volcanic Belt of SW Japan with high SiO_2( 52. 88% ~ 56. 89%),Mg O( 3. 47% ~ 6. 88%,Mg#ranging from 48. 5 to 63. 7),Sr( 442 × 10-6~ 970 × 10-6),Ba( 199 × 10-6~ 796 × 10-6),K/Na ranging from 0. 22 to 0. 70,P_2O_5 changing with a wide range( 0. 18% ~ 0. 52%). Moreover,all samples are enriched in large-ion lithophile elements and light rare earth elements(( La/Yb)N= 1. 88 ~ 15. 9),but strongly depleted in some high field strength elements( e. g. Nb,Ta and Hf) and heavy rare earth elements with slight negative Eu anomalies( δEu = 0. 77 ~ 0. 94). Additionally,the volcanic rocks have the same characteristics of Sr-Nd-Pb isotopes as typical sanukitoids((~(87)Sr/~(86)Sr)i= 0. 70366 ~ 0. 70409,(~(143)Nd/~(144)Nd)i= 0. 51247 ~0. 512564,εNd( t) = 4. 41 ~ 6. 19,~(206)Pb/~(204)Pb = 18. 220 ~ 18. 405,207Pb/~(204)Pb = 15. 482 ~ 15. 522,208Pb/~(204)Pb = 37. 991 ~38. 296). The confirmation of sanukitoids in Hala'alate Mountain proofs that it provides a new idea for studying the evolution of West Junggar,and provides important constraints on the remnant ocean basin closed time of West Junggar,meanwhile it indicate that the closed time should be postponed to the end of Late Carboniferous instead of the Early Carboniferous.
The Late Carboniferous volcanic rocks consist of basaltic andesite and pyroxene andesite which are widespread in Hala'alate Mountain,West Junggar. The volcanic rocks belong to calc-alkaline series and show a remarkable geochemical affinity with Cenozoic sanukitoids of the Setouchi Volcanic Belt of SW Japan with high SiO_2( 52. 88% ~ 56. 89%),Mg O( 3. 47% ~ 6. 88%,Mg#ranging from 48. 5 to 63. 7),Sr( 442 × 10-6~ 970 × 10-6),Ba( 199 × 10-6~ 796 × 10-6),K/Na ranging from 0. 22 to 0. 70,P_2O_5 changing with a wide range( 0. 18% ~ 0. 52%). Moreover,all samples are enriched in large-ion lithophile elements and light rare earth elements(( La/Yb)N= 1. 88 ~ 15. 9),but strongly depleted in some high field strength elements( e. g. Nb,Ta and Hf) and heavy rare earth elements with slight negative Eu anomalies( δEu = 0. 77 ~ 0. 94). Additionally,the volcanic rocks have the same characteristics of Sr-Nd-Pb isotopes as typical sanukitoids((~(87)Sr/~(86)Sr)i= 0. 70366 ~ 0. 70409,(~(143)Nd/~(144)Nd)i= 0. 51247 ~0. 512564,εNd( t) = 4. 41 ~ 6. 19,~(206)Pb/~(204)Pb = 18. 220 ~ 18. 405,207Pb/~(204)Pb = 15. 482 ~ 15. 522,208Pb/~(204)Pb = 37. 991 ~38. 296). The confirmation of sanukitoids in Hala'alate Mountain proofs that it provides a new idea for studying the evolution of West Junggar,and provides important constraints on the remnant ocean basin closed time of West Junggar,meanwhile it indicate that the closed time should be postponed to the end of Late Carboniferous instead of the Early Carboniferous.
引文
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