globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:5944298
论文题名:
陕西镇安二叠系碳酸盐岩粘土矿物特征及其对古气候的指示
其他题名: Clay Mineral Characteristics of Permian Carbonate Rocks in Zhen'an Area, Shaanxi Province and Its Paleoclimate Significance
作者: 曹婷丽; 程成; 李双应; 庞长兴; 魏星
刊名: 地质论评
ISSN: 0371-5736
出版年: 2017
卷: 63, 期:2, 页码:325-332
语种: 中文
中文关键词: 粘土矿物 ; 古气候 ; 二叠纪 ; 古特提斯洋 ; 陕西镇安
英文关键词: Clay mineral ; Palaeoclimate ; Permian ; Paleo-Tethys ; Zhen' ; an area in Shaanxi Province
WOS学科分类: MULTIDISCIPLINARY SCIENCES
WOS研究方向: Science & Technology - Other Topics
中文摘要: 二叠纪是地质历史中的一个关键时期,恢复其古气候具有重要意义。陕西镇安地区二叠纪时为古特提斯洋东部的一个孤立台地,二叠纪地层连续发育,厚度巨大(超过3 k_m),是研究二叠纪古气候古环境的理想之地。粘土矿物作为重要的古气候指标,可以恢复地质历史中的古气候。本次研究对陕西镇安二叠系159件碳酸盐岩样品进行了粘土矿物的定性和半定量分析,结果显示研究区粘土矿物组合为伊利石(平均含量70.9%)、高岭石(平均含量7.9%)、蒙脱石(平均含量4.4%)、绿泥石(平均含量8.6%)和伊蒙混层(平均含量8.3%)。伊利石相对含量变化显示研究区二叠纪古气候的变化可分为8个段:即阿舍尔期(Asselian)至空谷期(Kungurian)中期的干冷期(P1);中二叠世中期经历了湿热(P2)干冷(P3) 干冷暖湿交替(P4)的变化;卡匹敦期(Capitanian)中期至吴家坪期(Wuchiapingian)早期的气候变冷(P5);吴家坪期(Wuchiapingian)早期的短暂暖湿期(P6);吴家坪期(Wuchiapingian)早期至吴家坪期(Wuchiapingian)末期的气候逐渐变冷(P7);以及长兴期(Changhsingian)干冷暖湿交替显著的气候(P8)。同时,对比研究表明,研究区二叠纪古气候变化受晚古生代冰期事件(LPIA),Kamura事件及GLB(GuadalupianLopingian boundary)生物灭绝事件的影响。此外,研究区沃德期(Wordian)存在一个持续约2.4 Ma的短暂寒冷期,这与前人认为的空谷期(Kungurian)以来气候逐渐变暖不一致,其是否具有全球意义还有待进一步认识。
英文摘要: Objectives: Permian is a key period in geological history and the specific studies of Permian climate are scarce, so it's of great significance to further the study of paleoclimate. During Permian, the study area located in Zhen'an area in Shaanxi Province today, where Permian stratum is continuously developed and huge-thickly accumulated (more than 3 km),was an isolated platform in Eastern Paleo-Tethys. It's therefore a favorable profile to carry out the study on paleoclimate and paleoenvironment of Permian. Methods: 159 representative carbonate rock samples are picked out from the Permian section in Zhen'an area and then the qualitative and semiquantitative analysis of clay mineral are carried out. Results: The analysis shows that clay mineral of the study area is comprised of Illite (70.9%), Kaolinite (7.9%),Montmorillonite (4.4%),Chlorite (8.6%) and Illitesmectite mixed layer (8.3%). Based on the change of illite,s relative content,Permian palaeoclimate fluctuations in the study area can be divided into 8 phases: P1,from Asselian to middle Kungurian,was a drycold period; During the middle of Middle Permian, the climate fluctuated from warm--wet period (P2) to dry--cold period (P3), and to the alternation of dry-colding and warmweting (P4); P5, from middle Capitanian to early Wuchiapingian,was a cooling period; a short warmwet period happened in early Wuchiapingian (P6); an increasingly cooling period from early Wuchiapingian to the end of Wuchiapingian (P7); and an alternation of drycold and warmwet climate in Changhsingian (P8). Conclusions: The contrastive study among the study area,South China,Western Europe (Western Palaeo-Tethys) and Japan (Panthalassa) shows that the change of Permian palaeoclimate in Zhen' an area is influenced by the Late Paleozoic Ice Age (LPIA),Kamura Event and GLB biological extinction event. In addition,a short cold period (~2.4 Ma) during Wordian is identified by this study,which is different from previous views that the climate was gradually warming up from Kungurian onwards. Whether this phenomenon has global significance needs to be further studied.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/152349
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作者单位: 合肥工业大学资源与环境工程学院, 合肥, 安徽 230009, 中国

Recommended Citation:
曹婷丽,程成,李双应,等. 陕西镇安二叠系碳酸盐岩粘土矿物特征及其对古气候的指示[J]. 地质论评,2017-01-01,63(2):325-332
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