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Keyword [paleo-ocean]
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1. Mineral And Geochemical Characteristics Of The Cobalt-rich Crust(M38D-14) And Its Indication To Ancient Marine Environment
2. Geological Features Of Original Carbonate Veins In Chuanlinggou Formation And Their Paleo-oceanic Implications
3. The Palaeozoic Regional Tectonic Characteristics And Their Evolution Of The Western Segment Of Quruqtagh,Xinjiang
4. Cadmium Isotope Analytical Method And Its Paleo-ocean Environmental Significance
5. The Late Paleozoic Magmatism And Corresponding Iron And Copper Polymetallic Metallogenic In Kuokuqueke-Halegati District,Chinese Northwestern Tianshan
6. Trace Elements As Redox Paleoenvironments Proxies In Xiamaling Formation Of The Mesoproterozoic In North China And Their Geological Significances
7. Trace Elements As Redox Paleoenvironments Proxies In Chuanlinggou Formation Of The Mesoproterozoic In North China And Their Geological Significances
8. The Carbon Isotope Excursions And Paleo-oceanography Of The Ordovician-silurian Carbonate Rocks From The Xainza Area,Tibet
9. The Oxygenation Events And The Multicellularization Of Eukaryote In Mesoproterozoic Gaoyuzhuang Formation In Jixian North China
10. Research On The Paleo-ocean Environments Of Gaoyuzhuang Formation,Yanqing Area,North China
11. The Characteristics Of ?13C In The Third Section Of Doushantuo Formation In South China And The Indication Of The Paleo-ocean Redox Conditions
12. Middle Permian Paleo-ocean Environmental Evolution And Cause Mechanisms Of The Capitanian Mass Extinction In The Lower Yangtze Region
13. The Effects Of Multiple Diagenesis On Carbonate Mg Isotopes And Application On Reconstruction Of Paleo-Marine Environments Changes
14. Geochemical Characteristics Of The Black Shales From The Shuijingtuo Formation In The Shennongjia Area And Their Paleoenvironmental Implications
15. Fe Speciation Of Cherts Near The Ediacaran-Cambrian Boundary Of The Pingyin Section In South China And Its Paleo-ocean Environmental Significance
16. The Paleo-ocean Environment Evolution Of Early Cambrian And Its Influence On Organic Matter Enrichment Model In Northern Guizhou
17. The Evolution Of The Paleo-ocean Environment Revealed By Planktonic Foraminifera Since 70 Ka In The Mid-latitude North Atlantic
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