Presentation is loading. Please wait.

Presentation is loading. Please wait.

Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure S-3 Backscattered electrons SEM image and SEM-EDXS.

Published byHugues Cartier Modified over 6 years ago

Similar presentations

Presentation on theme: "Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure S-3 Backscattered electrons SEM image and SEM-EDXS."— Presentation transcript:

1 Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure S-3 Backscattered electrons SEM image and SEM-EDXS analysis of Th-monazite in the 2012_ cm sediment samples. Corresponding semi-quantitative analyses are reported in Table S-2. Figure S-3 Backscattered electrons SEM image and SEM-EDXS analysis of Th-monazite in the 2012_ cm sediment samples. Corresponding semi-quantitative analyses are reported in Table S-2. Morin et al. (2016) Geochem. Persp. Let. 2, | doi: /geochemlet.1610 © 2016 European Association of Geochemistry

Download ppt "Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure S-3 Backscattered electrons SEM image and SEM-EDXS."

Similar presentations

UWO Nanofabrication Facility and Science Studio. Facility to be hooked into Science Studio: Western Nanofabrication Facility, University of Western Ontario.

UWO Nanofabrication Facility and Science Studio. Facility to be hooked into Science Studio: Western Nanofabrication Facility, University of Western Ontario.
P449. p450 Figure 15-1 p451 Figure 15-2 p453 Figure 15-2a p453.

P449. p450 Figure 15-1 p451 Figure 15-2 p453 Figure 15-2a p453.
Figure S-2 Zircon U-Pb age distribution for detrital zircons from North & Central America, Australia, Europe, South America, Africa, Asia and India using.

Figure S-2 Zircon U-Pb age distribution for detrital zircons from North & Central America, Australia, Europe, South America, Africa, Asia and India using.
P247. Figure 9-1 p248 Figure 9-2 p251 p251 Figure 9-3 p253.

P247. Figure 9-1 p248 Figure 9-2 p251 p251 Figure 9-3 p253.
Figure 18-1. Figure 18-1 part 1 Figure 18-1 part 2.

Figure Figure 18-1 part 1 Figure 18-1 part 2.
1 times table 2 times table 3 times table 4 times table 5 times table

1 times table 2 times table 3 times table 4 times table 5 times table
$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.

$100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300.
Tables Learning Support

Tables Learning Support
Image from

Image from
Figure 3 from Interannual variability of nitrogen oxides emissions from boreal fires in Siberia and Alaska during 1996–2011 as observed from space (Image.

Figure 3 from Interannual variability of nitrogen oxides emissions from boreal fires in Siberia and Alaska during 1996–2011 as observed from space (Image.
Creech et al. Late accretion history of the terrestrial planets inferred from platinum stable isotopes Figure 3 Model of the effect of addition of chondritic.

Creech et al. Late accretion history of the terrestrial planets inferred from platinum stable isotopes Figure 3 Model of the effect of addition of chondritic.
The solubility of heat-producing elements in Earth’s core

The solubility of heat-producing elements in Earth’s core
Distribution of Zn isotopes during Alzheimer’s disease

Distribution of Zn isotopes during Alzheimer’s disease
Direct sensing of total alkalinity profile in a stratified lake

Direct sensing of total alkalinity profile in a stratified lake
Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a)

Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a)
Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure S-3 Reconstructed Ba/Th vs. La/Sm ratios for.

Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure S-3 Reconstructed Ba/Th vs. La/Sm ratios for.
Dahl et al. Reorganisation of Earth’s biogeochemical cycles briefly oxygenated the oceans 520 Myr ago Figure 3 Conceptual model for the episodic expansion.

Dahl et al. Reorganisation of Earth’s biogeochemical cycles briefly oxygenated the oceans 520 Myr ago Figure 3 Conceptual model for the episodic expansion.
Schiller et al. Tracking the formation of magma oceans in the Solar System using stable magnesium isotopes Figure 1 The minimum degree of partial melting.

Schiller et al. Tracking the formation of magma oceans in the Solar System using stable magnesium isotopes Figure 1 The minimum degree of partial melting.
Telocytes: Connective tissue repair and communication cells

Telocytes: Connective tissue repair and communication cells
Opportunities in Italy and Europe

Opportunities in Italy and Europe

Similar presentations

Ads by Google