西藏南部吉隆盆地中新世—早更新世孢粉组合带及其地质意义

徐亚东; 张克信; 王国灿; 向树元; 江尚松; 陈奋宁

doi:10.3799/dqkx.2010.090

西藏南部吉隆盆地中新世—早更新世孢粉组合带及其地质意义

doi: 10.3799/dqkx.2010.090

徐亚东^{1, 2,},
张克信^{1, 2, ,},
王国灿^{2, 3},
向树元²,
江尚松²,
陈奋宁⁴

1.
中国地质大学生物地质与环境地质教育部重点实验室, 湖北武汉 430074
2.
中国地质大学地球科学学院, 湖北武汉 430074
3.
中国地质大学地质过程与矿产资源国家重点实验室, 湖北武汉 430074
4.
西安地质矿产研究所, 陕西西安 710054

基金项目:

中国地质调查局项目 1212010610103

国家自然科学基金项目 40830212

国家自然科学基金项目 40921062

详细信息

作者简介:
徐亚东(1983-), 男, 博士研究生, 从事地层古生物等研究.E-mail: yuren36@gmail.com

通讯作者:
张克信, E-mail: kx_zhang@cug.edu.cn

中图分类号: P534
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出版历程
- 收稿日期: 2010-05-31
- 刊出日期: 2010-09-01

Geological Significance of Miocene-Early Pleistocene Palynological Zones in the Gyirong Basin, Southern Tibet

1.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faulty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

摘要

摘要: 吉隆盆地为高喜马拉雅中新世晚期约10 Ma时期形成的一个南北向断陷盆地, 其东侧为同沉积正断层, 沃马剖面位于盆地沉降中心的东南部.在该剖面下部新发现一套中新世巨厚砾岩层(旦增竹康组).通过锆石和磷灰石裂变径迹年代学研究得出吉隆盆地控盆断裂早期活动时间为13.4±1.9 Ma, 源区12~11 Ma发生构造热事件, 据此推算出吉隆盆地初始裂陷后开始沉积的底界年龄约为10 Ma.综合前人在吉隆盆地得出的7.20~1.67 Ma古地磁测年值, 可得出吉隆盆地旦增竹康组年龄为10.0~7.4 Ma, 沃马组年龄为7.40~1.67 Ma.根据孢粉组合带和孢粉组合反映的植物类型和古环境变化, 沿剖面自下而上划分为3个孢粉组合带和9个孢粉组合及其对应的植被类型.吉隆地区古气候变化可划分为3个阶段: (1)组合带Ⅰ和孢粉组合1~2, 为温暖偏干环境的常绿与落叶针阔叶混交林, 地层对比时代为晚中新世(10.0~7.0 Ma); (2)组合带Ⅱ和孢粉组合3~7, 为寒冷干旱环境的落叶针叶林, 期间存在一次暖湿气候的波动, 地层对比时代为晚中新世晚期-早上新世(7.0~3.3 Ma); (3)组合带Ⅲ和孢粉组合8~9, 为温凉偏干的气候下生长暗针叶林和落叶阔叶林构成的针阔叶混交林, 地层对比时代为晚上新世(3.30~1.67 Ma).
- 青藏高原 /
- 吉隆盆地 /
- 孢粉组合 /
- 古气候变化 /
- 新近纪
Abstract: The Gyirong basin is one of east-west extensional basins distributed among the high Himalayas. The Late Cenozoic sequence is mainly Woma Formation, consisting of lacustrine and fluvial deposits, from which a Hipparion fauna in 7 Ma was found. However, Danzengzhukang Formation is newly found at the base of the section attributed to alluvial sequence. The zircon and apatite fission track thermochronology shows that eroded source experienced tectonic thermal event at 12-11 Ma, and early activity of the east boundary normal fault of the basin occurred during 13.4±1.9 Ma. Based on the previous paleomagnetostratigraphic researches of the basin, the age interval of the section is most reasonably determined as between 10 and 1.67 Ma. Through abundant palynological analyses, 3 palynological zones and 9 palynological assemblages and vegetable types are recognized, and 3 phases of paleoclimatic changes are revealed: (1) 10.0-6.7 Ma, correlating with palynological zone Ⅰ and assemblages 1-2, it was warm and damp-dry coniferous-leaved and broad-leaved mixed forests, but became cool and humid during 9.5-7.0 Ma. (2) 6.7-3.3 Ma, correlating with palynological zone Ⅱ and assemblages 3-7, it turned cold and arid deciduous coniferous-leaved forests, marked by the increase in the cold-tolerant tree taxa and drought-tolerant herb taxa, but the relative increase of broad-leaved taxa suggests climate underwent warm and humid fluctuations during 5.0-4.3 Ma. (3) 3.30-1.67 Ma, correlating with palynological zone Ⅲ and assemblages 8-9, it got cool and damp-dry deciduous coniferous-leaved and broad-leaved mixed forests.
- Qinghai-Tibetan plateau /
- Gyirong basin /
- palynological assemblage /
- paleoclimate change /
- Neogene

HTML全文

图 1 西藏吉隆沃马剖面交通位置与地质简图

1.全新统；2.更新统；3.中新统-下更新统沃马组；4.中新统旦增竹康组；5.上侏罗统门卡墩组；6.中侏罗统拉弄拉组/聂聂雄拉组；7.下-中侏罗统日当组；8.一般地质界线；9.角度不整合、平行不整合界线；10.正断层；11.逆断层；12.性质不明断层；13.县行政所在地；14.村镇；15.居民点；16.公路；17.简易公路；18.河流

Fig. 1. Location and geological map showing the study Oma Section in the Gyirong basin in Tibet, China

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图 2 西藏吉隆沃马剖面新近系旦增竹康组—沃马组地层柱状图

1.平行层理; 2.水平层理; 3.板状交错层理; 4.楔状交错层理; 5.叠瓦状构造; 6.砂砾石透镜体; 7.砾岩; 8.含砾砂岩; 9.砂岩; 10.粉砂岩; 11.泥质粉砂岩; 12.粉砂质泥岩、泥岩; 13.三趾马动物群化石点. Af.冲积扇; fr-fe.扇根-扇端; Rb.河流; rb-fp河床-泛滥平原; Fd.扇三角洲; fdp.扇三角洲平原; fdp-fdm.扇三角洲平原-前缘; L.湖泊; k1.滨湖; sl.浅湖; d1.深湖

Fig. 2. Composite strata column section of Neogene Danzengzhukang Formation and Oma Formation in Gyirong basin, Tibet

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图 3 吉隆沃马剖面蕨类和裸子植物孢子主要类型属种化石

1.凤尾蕨Pteris sp.；样品号：S₂BF62-6(71)；2.瘤足蕨Plagiogyria sp.；样品号：S₂BF62-6(71)；3.海金沙Lygodium sp.；样品号：S₂BF62-7(72)；4.水龙骨Polypodium sp.；样品号：S₂BF62-7(72)；5.罗汉松Podocarpus sp.；样品号：S₂BF88-5(44)；6.松Pinus sp.；样品号：S₁BF14-1(6)；7.无囊铁杉Tsuga sp₁.；样品号：S₁BF14-1(6)；8.具周囊铁杉Tsuga sp₂.；样品号：S₂BF62-7(72)；9.雪松Cedrus sp.；样品号：S₁BF22-1(13)；10.云杉Picea sp.；样品号：S₁BF22-1(13)；11.冷杉Abies sp.；样品号：S₁BF14-1(6)

Fig. 3. Representative photographs of fern and gymnosperm spore grains from the Oma Section in the Gyirong basin

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图 4 吉隆沃马剖面被子植物花粉主要类型属种化石

1.柳Salix sp.；样品号：S₂BF63-6(82)；2.楝Melia sp.；样品号：S₂BF48-3(47)；3.鹅耳枥Carpinus sp.；样品号：S₁BF14-1(6)；4.榛Corylns sp.；样品号：S₂BF96-4(50)；5.常绿栎Quercus evergreen；样品号：S₂BF48-3(47)；6.落叶栎Quercus deciduous.；样品号：S₂BF48-3(47)；7.桤木Alnus sp.；样品号：S₁BF22-1(13)；8.桦Betula sp.；样品号：S₁BF14-1(6)；9.枫杨Pterocarya sp.；样品号：S₂BF96-4(50)；10.胡桃Juglans sp.；样品号：S₂BF62-7(72)；11.椴Tilia sp.；样品号：S₂BF48-4(48)；12.蒿Artemisia sp.；样品号：S₁BF15-1(7)；13.菊科Compositae；样品号：S₂BF36-2(30)；14.藜Chenopodium sp.；样品号：S₁BF14-1(6)

Fig. 4. Representative photographs of angiosperm pollen grains from the Oma Section in Gyirong basin

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图 5 西藏吉隆沃马剖面中-上新世孢粉谱

Fig. 5. Overview of the palynological diagram and major vegatation changes during the Mio-Pliocene in the Gyirong basin

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图 6 吉隆盆地新近纪孢粉组合带及其划分对比

Fig. 6. Neogene palynological zones of Gyirong basin and its division and correlation with other sequences

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