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中国地质大学科学技术发展院邱轩(BGEG国家重点实验室), 王红梅*(环境学院)等 Earth and Planetary Science Letters,2017. High salinity facilitates dolomite precipitation mediated by Haloferax volcanii DS52
白云岩;沉积岩;高盐度
2021/10/21
2017年6月,中国地质大学王红梅教授团队的研究成果——高盐度促进Haloferax volcaniiDS52介导形成白云石(High salinity facilitates dolomite precipitation mediated byHaloferax volcaniiDS52)发表在地学领域Nature Index的期刊《Earth and Planetary Science Let...
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Professor Joe Cartwright,Department of Earth Sciences at University of Oxford(图)
Professor Joe Cartwright Department of Earth Sciences at University of Oxford depositional diagenetic deformational
2014/3/10
Sedimentary Processes on Earth, Mars, Titan, and Venus
Sedimentary Processes Earth Mars Titan Venus
2014/4/8
The production, transport and deposition of sediment occur to varying degrees on Earth, Mars, Venus, and Titan. These sedimentary processes are significantly influenced by climate that affects product...
Rare earth elements in the ornithogenic sediments from the Maritime Antarctic: A potential new palaeoecology proxy
Antarctica ornithogenic sediments rare earth elements
2017/4/12
The ornithogenic sediments in the maritime Antarctic are good archives for studying the changes of historical penguin
population. Rare earth elements (REEs) along with biological and lithophile eleme...
从黔南、桂北的航天遥感图像上可以清楚地看出,地表的宏观岩溶地貌明显地受控于区域性大型“X”共轭节理系统,此类节理构成一幅巨型的渗滤网,成为大气降水下渗的主要通道,从而导致被其穿透的岩石遭受溶蚀,形成以线性岩溶谷地为主体的岩溶景观。即水平地层分布区,呈片状“X”形网络结构;直立地层分布区,呈羽状条带结构。水体下渗至潜水面后,将主要沿“X”节理走向向当地最低侵蚀基准面排泄,从而形成复杂的地下管道网络系...
从黔南、桂北的航天遥感图像上可以清楚地看出,地表的宏观岩溶地貌明显地受控于区域性大型“X”共轭节理系统,此类节理构成一幅巨型的渗滤网,成为大气降水下渗的主要通道,从而导致被其穿透的岩石遭受溶蚀,形成以线性岩溶谷地为主体的岩溶景观。即水平地层分布区,呈片状“X”形网络结构;直立地层分布区,呈羽状条带结构。水体下渗至潜水面后,将主要沿“X”节理走向向当地最低侵蚀基准面排泄,从而形成复杂的地下管道网络系...