洞穴石笋纹(壳)层层组类型研究

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洞穴石笋纹(壳)层层组类型研究

张美良, 林玉石, 覃嘉铭

文章导航 > 沉积学报 > 2002 > 20(3): 435-441

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

引用本文:

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

Citation:

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

引用本文:

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

Citation:

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

洞穴石笋纹(壳)层层组类型研究

中国地质科学院岩溶地质研究所,岩溶动力学开放研究实验室,广西桂林,541004

基金项目: IGCP-448国际对比项目科技部攀登特别资助项目“全球岩溶生态系统对比”(编号:2000-026)国家自然科学基金项目(批准号:40152002)资助

作者简介:
张美良,男,1956年出生,高级工程师,区域岩溶或古环境研究?

中图分类号: P642.25

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文章访问数: 821
HTML全文浏览量: 129
PDF下载量: 715
被引次数: 0

Study on Laminae or Lamella Groups and Types of Stalagmite in Caves

Institute of Karst Geology,CAGS,Guilin Guangxi,541004

摘要: 石笋是洞穴碳酸钙沉积的典型滴石类型,也是岩溶记录中最全面、最系统的古气候环境信息载体,随着高分辨率测年技术和测试方法的提高,它在重建古气候环境方面具有重要的意义.石笋沉积纹层的组合、厚度、粒度和层面构造等,是恢复成笋滴水动态及相关古水文条件的物质基础,其中不少古气候环境信息,具强烈直观感,聚集物证、形象地记录于石笋剖面中,易观测研究.通过大量石笋纵剖面观测和系统的同位素组成、微(痕)量元素、特征性纹层的分析研究,证实石笋沉积纹(壳)层具韵律性组合和沉积旋回性及其古气候环境显示.首次提出石笋具叠锥型、叠柱型、叠锥叠柱复(组)合型纹(壳)层组和连续性、旋回性、间断(歇)性叠复纹(壳)层层组类型的沉积构造,并阐述各自的特征、滴流水动态和气候环境演变特征。
- 洞穴石笋 /
- 沉积纹(壳)层 /
- 层组类型 /
- 古气候环境
Abstract: Stalagmite is a typical dripstone shape of CaC0₃ in caves and the most comprehensive and systematical paleoclimate environment in for mation carrier too. With advances of dating techniCues and analytic methods with high resolution，it is of great significance in the paleoclimate environment reconstruction. The combi nation，thickness，grain size and bedding plane structure of depositional laminae in stalagmite are the material base to resume droping water trends of for ming stalagmite and the related paleo- hydrological conditions. 0n the basis of the analysis and study of many stalagmite vertical profiles and systematic isotopic compositions,trace elements and specific laminae，it has been demonstrated that stalagime sedimentary laminae have obvious rhythmic combination,sedimentary cycles and indication of paleoclimatic environments. It is firstly put for ward that stalagmite is of lamina groups of cone in cone,cone and pillar,cone i n cone and pillar combined types and with the sediment ary structures,such as continuity,cycle,disconnected and compound lamina types. The paper discusses their indivitual charatersitics，trends of dropping and flow water and evolutionary characteristics of climatic environments.
- cave stalagmite /
- sediment laminae /
- lamina types /
- paleoclimatic environment

参考文献(16)

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[4]	杨明德, 谭明, 梁虹. 喀斯特流域水文地貌系统[M]. 北京:地质出版社,1998.24～34[ Yang Mingde,Tan Ming,Liang Hong.Hydrogeomorphologicial system of karst drainage basin[M]. Beijing: Geological publishing house,1998.24～34]
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[7]	李红春, 顾德隆, 陈文寄.利用洞穴石笋的δ^18O和δ¹³C重建3000年以来北京地区气候和古环境-石花洞研究系列之三[J]. 地震地质, 1997,19(1):71～85 [Li Hongchun, Ku The-lung, Chen Wenji, et al. Isotope studies of Shihua cave-Ⅲ:Reconstruction of paleoclimate and paleoenvironment of Beijing during the Last 3000 years from δ^18O and δ¹³C records in stalagmite[J]. Seismology And Geology,1997,19(1):77～86]
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文章访问数: 821
HTML全文浏览量: 129
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洞穴石笋纹(壳)层层组类型研究

中国地质科学院岩溶地质研究所,岩溶动力学开放研究实验室,广西桂林,541004

基金项目: IGCP-448国际对比项目科技部攀登特别资助项目“全球岩溶生态系统对比”(编号:2000-026)国家自然科学基金项目(批准号:40152002)资助

作者简介:
张美良,男,1956年出生,高级工程师,区域岩溶或古环境研究?

收稿日期: 2001-05-28
修回日期: 2001-08-30

中图分类号: P642.25

关键词:

沉积纹(壳)层 /

古气候环境

摘要: 石笋是洞穴碳酸钙沉积的典型滴石类型,也是岩溶记录中最全面、最系统的古气候环境信息载体,随着高分辨率测年技术和测试方法的提高,它在重建古气候环境方面具有重要的意义.石笋沉积纹层的组合、厚度、粒度和层面构造等,是恢复成笋滴水动态及相关古水文条件的物质基础,其中不少古气候环境信息,具强烈直观感,聚集物证、形象地记录于石笋剖面中,易观测研究.通过大量石笋纵剖面观测和系统的同位素组成、微(痕)量元素、特征性纹层的分析研究,证实石笋沉积纹(壳)层具韵律性组合和沉积旋回性及其古气候环境显示.首次提出石笋具叠锥型、叠柱型、叠锥叠柱复(组)合型纹(壳)层组和连续性、旋回性、间断(歇)性叠复纹(壳)层层组类型的沉积构造,并阐述各自的特征、滴流水动态和气候环境演变特征。

English Abstract

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

引用本文:

张美良, 林玉石, 覃嘉铭. 洞穴石笋纹(壳)层层组类型研究[J]. 沉积学报, 2002, 20(3): 435-441.

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

Citation:

ZHANG Mei-liang, LIN Yu-shi, QIN Jia-ming. Study on Laminae or Lamella Groups and Types of Stalagmite in Caves[J]. Acta Sedimentologica Sinica, 2002, 20(3): 435-441.

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