Search alternatives:
ms decrease » _ decrease (Expand Search), nn decrease (Expand Search), use decreased (Expand Search)
we decrease » _ decrease (Expand Search), nn decrease (Expand Search), teer decrease (Expand Search)
a decrease » _ decrease (Expand Search), _ decreased (Expand Search), _ decreases (Expand Search)
ms decrease » _ decrease (Expand Search), nn decrease (Expand Search), use decreased (Expand Search)
we decrease » _ decrease (Expand Search), nn decrease (Expand Search), teer decrease (Expand Search)
a decrease » _ decrease (Expand Search), _ decreased (Expand Search), _ decreases (Expand Search)
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44761
Data_Sheet_1_Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland).docx
Published 2018“…Olivine (Ol) is classified into two groups based on its forsterite content: (1) Fo<sub>88.9−91.5</sub>, which accounts for a fertile-to-residual mantle, and (2) Fo<sub>85.5−88.1</sub>, which indicates large interactions with circulating (basic) melts. …”
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44762
Image_3_Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland).JPEG
Published 2018“…Olivine (Ol) is classified into two groups based on its forsterite content: (1) Fo<sub>88.9−91.5</sub>, which accounts for a fertile-to-residual mantle, and (2) Fo<sub>85.5−88.1</sub>, which indicates large interactions with circulating (basic) melts. …”
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44763
Image_7_Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland).JPEG
Published 2018“…Olivine (Ol) is classified into two groups based on its forsterite content: (1) Fo<sub>88.9−91.5</sub>, which accounts for a fertile-to-residual mantle, and (2) Fo<sub>85.5−88.1</sub>, which indicates large interactions with circulating (basic) melts. …”
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