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Groundwater Systems and Resources in the Ordos Basin, ChinaOA

Groundwater Systems and Resources in the Ordos Basin, China

中文摘要英文摘要

The Ordos Basin is.a large-scalesedimentary basin in northwestern China. The hydrostratigraphic units from bottom to top are pre-Cambrian metamorphic rocks, Lower Paleozoic carbonate rocks, Upper Paleozoic to Mesozoic clastic…查看全部>>

The Ordos Basin is.a large-scalesedimentary basin in northwestern China. The hydrostratigraphic units from bottom to top are pre-Cambrian metamorphic rocks, Lower Paleozoic carbonate rocks, Upper Paleozoic to Mesozoic clastic rocks and Cenozoic deposits. The total thickness is up to 6000 m. Three groundwater systems are present in the Ordos Basin, based on the geological settings, I.e. The karst groundwater system, the Cretaceous dastic groundwater system an…查看全部>>

HOU Guangcai;LIANG Yongping;SU Xiaosi;ZHAO Zhenghong;TAO Zhengping;YIN Lihe;YANG Yuncheng;WANG Xiaoyong

Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin, Guangxi 541004Institute of Water Resources and Environment, Jilin University, Changchun, Jilin 130026Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054Xi'an Institute of Geology and Mineral Resources, Xi'an, Shaanxi 710054

天文与地球科学

groundwater systemcirculation and evolutiongroundwater resourcesOrdos Basin

groundwater systemcirculation and evolutiongroundwater resourcesOrdos Basin

《地质学报(英文版)》 2008 (5)

1061-1069,9

This work was supported by grants from the Chinese Geological Survey Plan(No.1212010331302)and IAEA Technical Cooperation Project (CPR/012-017).Drs.Yin Yueping,Wu Xuanmin and Wen Dongguang are deeply appreciated for their support.We are very grateful to Profs.Wang Deqian,Liu Fang,Drs.Zhang Maosheng,Wang Yonghe and our colleagues for their valuable comments.

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