CAJ | 학술논문

北祁连构造带1∶5万水系沉积物测量元素Ag、As、Au、Ba、Bi、Co、Cr、Cu、Fe、Hg、Mo、Mn、Ni、Pb、Sn、Sb、Ti、W、Zn，其异常特征在不同地质时代随构造环境的演化而变化，与放射性同位素地球化学一样，水系沉积物元素自身在本质上包含了时间和构造背景的双重属性。通过衬值法对不同时代地层中的49303个大数据样本元素含量原始数据进行处理，结合用以探讨地层元素地球化学特征的R型聚类分析进行分组研究。结果表明：北祁连造山带中Co、Cr、Ni的水系沉积物元素异常响应于古元古代之后造山带的裂解构造环境；Au、Bi 和部分Cu异常与奥陶纪大洋的俯冲—闭合阶段构造环境对应；Pb、Zn异常可能是奥陶—志留纪北祁连弧盆体系中局部洋底火山活动中的热液喷流形成；泥盆系Hg、Sb异常尚无区域上合理的构造环境来解释；Mo含量于石炭系出现峰值，说明北祁连造山带周边处于强烈抬升剥蚀；W、Sn异常反映了奥陶纪、志留纪俯冲碰撞的构造背景。这种水系沉积物测量元素异常特征与构造带构造演化阶段同步响应的规律性表明，水系沉积物测量中幔源元素的相容（不相容）特性可很好地判别单一旋回造山带的构造环境，采用大数据样本将勘查地球化学理论拓展应用于大地构造学研究是可行的。
북기련구조대1∶5만수계침적물측량원소Ag、As、Au、Ba、Bi、Co、Cr、Cu、Fe、Hg、Mo、Mn、Ni、Pb、Sn、Sb、Ti、W、Zn，기이상특정재불동지질시대수구조배경적연화이변화，여방사성동위소지구화학일양，수계침적물원소자신재본질상포함료시간화구조배경적쌍중속성。통과츤치법대불동시대지층중적49303개대수거양본원소함량원시수거진행처리，결합용이탐토지층원소지구화학특정적R형취류분석진행분조연구。결과표명：북기련조산대중Co、Cr、Ni적수계침적물원소이상향응우고원고대지후조산대적렬해구조배경；Au、Bi 화부분Cu이상여오도기대양적부충—폐합계단구조배경대응；Pb、Zn이상가능시오도—지류기북기련호분체계중국부양저화산활동중적열액분류형성；니분계Hg、Sb이상상무구역상합리적구조배경래해석；Mo함량우석탄계출현봉치，설명북기련조산대주변처우강렬태승박식；W、Sn이상반영료오도기、지류기부충팽당적구조배경。저충수계침적물측량원소이상특정여구조대구조연화계단동보향응적규률성표명，수계침적물측량중만원원소적상용（불상용）특성가흔호지판별단일선회조산대적구조배경，채용대수거양본장감사지구화학이론탁전응용우대지구조학연구시가행적。
Elements anomalies, such as Ag, As, Au, Ba, Bi, Co, Cr, Cu, Fe, Hg, Mo, Mn, Ni, Pb, Sn, Sb, Ti, W, Zn, from 1∶50 000 stream sediment survey, North Qilian tectonic belt, vary with the tectonic evolution in different geological epochs , the ele?ments themselves are endowed with dual properties of time and tectonic setting. According to the contrast value method, element content data of 49 303 samples from different strata were processed in combination with stratigraphic geochemical R cluster grouping. The results show that Co, Cr, Ni anomalies are in response to Paleoproterozoic post?orogenic cracking, Au, Bi and part of Cu anomalies are in re?sponse to Ordovician oceanic subduction?closing stages, Pb, Zn anomalies probably corresponded to local volcanic activity in the ocean floor in Ordovician?Silurian period. Devonian Hg, Sb anomalies have no reasonable regional tectonic interpretation, and the phenomenon of Mo element content in the Carboniferous peak indicates strong uplift and erosion on the periphery of North Qilian oro?genic belt. W, Sn element anomalies reflect subduction and collision setting in Ordovician and Silurian. The regularity of the stream sediment anomalies'response to tectonic evolution suggests that the compatible ( incompatible ) features of mantle?derived elements from stream sediment survey can better distinguish tectonic environments, and the combinational geochemical approach from a large data sample and tectonic study is feasible.