| 太湖沉积物-水界面生源要素迁移机制及定量化—2.磷释放的热力学机制及源-汇转换 |
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| 引用本文： | 范成新,张路,包先明,尤本胜,钟继承,王建军,丁士明.太湖沉积物-水界面生源要素迁移机制及定量化—2.磷释放的热力学机制及源-汇转换[J].湖泊科学,2006,18(3):207-217. |
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| 作者姓名： | 范成新 张路 包先明 尤本胜 钟继承 王建军 丁士明 |
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| 作者单位： | 1. 中国科学院南京地理与湖泊研究所,南京,210008;中国科学院研究生院,北京,100039
2. 中国科学院南京地理与湖泊研究所,南京,210008 |
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| 基金项目： | 国家高技术研究发展计划(863计划) |
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| 摘 要： | 通过对云贵高原西北部鹤庆钻孔古湖相沉积岩芯的粒度、碳酸盐含量和烧失量等指标的综合分析、研究,重建了鹤庆盆地2．78 Ma以来的古环境演化过程．岩芯磁性地层表明,鹤庆湖盆形成于约2．78 Ma．环境代用指标的综合分析显示:鹤庆盆地2．78 Ma以来有过三次大的环境转变,即2．65 Ma鹤庆湖盆积水成湖,1．55 Ma、0．99 Ma左右山盆高差两次加大,这分别与青藏运动B幕、C幕和昆黄运动耦合．
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| 关 键 词： | 构造运动 多指标综合分析 环境演变 鹤庆盆地 |
| 收稿时间： | 2005-04-06 |
| 修稿时间： | 2005-08-03 |
Paleoenvironmental evolution of Heqing basin in Yunnan Province since 2.78 Ma |
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| FAN Chengxin,ZHANG Lu,BAO Xianming,YOU Bensheng,ZHONG Jicheng,WANG Jianjun and DING Shiming.Paleoenvironmental evolution of Heqing basin in Yunnan Province since 2.78 Ma[J].Journal of Lake Science,2006,18(3):207-217. |
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| Authors: | FAN Chengxin ZHANG Lu BAO Xianming YOU Bensheng ZHONG Jicheng WANG Jianjun and DING Shiming |
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| Institution: | 1.Nanjing Institute of Geography and Limnology, CAS, Naning 210008 ,P. R. China; 2. Graduate School, CAS, Beijing 100039, P. R. China |
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| Abstract: | Based on multi-proxy investigations such as grain size, content of carbonate and loss on ignition of the deep core of the ancient lake in the Heqing basin, the northwest of Yungui Plateau, it is reconstructed for a 2. 78 Ma paleoenvironmental evolution. The result of magnetic stratum indicates that the Heqing lake basin was formed at about 2.78 Ma. Further, the multi-proxy analysis reveals that there had been three major environmental stages in the Heqing basin since 2. 78 Ma, namely the lake basin accumulated water to be a lake in 2. 65 Ma,and the height difference between the mountains and basin increased twice at about 1. 55 Ma and 0.99 Ma. These stages couples well with Qingzang movement phase B, phase C and Kunlun-Huanghe movement respectively. |
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| Keywords: | tectonic movement multi-proxy investigations environmental evolution Heqing basin |
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