Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a)

Slides:



Advertisements
Similar presentations
Phase diagrams for melting in the Earth (101): thermodynamic fundamentals Jan Matas Université de Lyon Ecole normale supérieure de Lyon, CNRS CIDER 2010.
Advertisements

Reading: Winter (2001) Chapter 18
30 years of P-T-t paths: What we’ve learned about orogenesis
Figure S-2 Zircon U-Pb age distribution for detrital zircons from North & Central America, Australia, Europe, South America, Africa, Asia and India using.
WATER-ICE CONTENT IN TITAN AND CALLISTO Dunaeva A.N., Kronrod V.A., Kuskov O.L. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy.
Water in the Mantle ? Can be stored: 1)Hydrous minerals - only stable shallow 2) Dissolved in normally anhydrous minerals 3)A hydrous silica-rich fluid.
Plate Tectonics Review $100 $100 $200 $200 $300 $300 $400 $400 $500 $500 $100 $100 $200 $200 $300 $300 $400 $400 $500 $500 $100 $100 $200 $200 $300 $300.
Date of download: 5/29/2016 Copyright © ASME. All rights reserved. From: A Study on the Optimization of an Air Dehumidification Desiccant System J. Thermal.
1. Inner Core Outer Core Mantle Crust 2  The Earth's outermost surface is called the crust. The crust is typically about 25 miles thick beneath continents,
Radiative Thermal Conductivity of the Lower Mantle Emma Rainey Abby Kavner Laurent Pilon.
What is the thermal structure of a subduction zone?
Date of download: 7/9/2016 Copyright © 2016 SPIE. All rights reserved. Schematic diagram of the coordinate system; θ is the viewing angle and O.R. represents.
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
Distribution of Zn isotopes during Alzheimer’s disease
Date of download: 10/15/2017 Copyright © ASME. All rights reserved.
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 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.
The Rock Cycle.
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.
Douglas A. Wiens & James Conder
Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure 4 (a) Concentration of U(IV) extracted by O2-free.
Squeezing the Slab: future directions for metamorphic petrology in the SZO Andrew Smye Sentence about metamorphic petrology and need to link observations.
Tartèse et al. Warm Archaean oceans reconstructed from oxygen isotope composition of early-life remnants Figure 2 (a) Comparison of the chert and calculated.
Savage et al. Copper isotope evidence for large-scale sulphide fractionation during Earth’s differentiation Figure 2 Schematic evolution of Cu concentration.
Date of download: 11/7/2017 Copyright © ASME. All rights reserved.
Schmidt and Manning Pressure-induced ion pairing in MgSO4 solutions: Implications for the oceans of icy worlds Figure S-2 Percentage of contact ion pairs.
Date of download: 11/8/2017 Copyright © ASME. All rights reserved.
Date of download: 11/9/2017 Copyright © ASME. All rights reserved.
Compositional symmetry between Earth’s crustal building blocks
Compositional symmetry between Earth’s crustal building blocks
Date of download: 11/11/2017 Copyright © ASME. All rights reserved.
Rapid cooling of planetesimal core-mantle
Giunta et al. The gravitas of gravitational isotope fractionation revealed in an isolated aquifer Figure 1 Isotope ratios and concentrations co-variations.
Evidence of sub-arc mantle oxidation by sulphur and carbon
From: Development of a Coring Test for Non-Coring Huber Needles
Figure S-1 Map of the study area
Rivas-Lamelo et al. Magnetotactic bacteria as a new model for P sequestration in the ferruginous Lake Pavin Figure 1 Scanning transmission electron microscopy.
A cometary origin for martian atmospheric methane
Hawkings et al. The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet Figure S-4 Comparison of regression plots for.
Hydrocarbons as ore fluids
Savage et al. Copper isotope evidence for large-scale sulphide fractionation during Earth’s differentiation Figure S-6 Relationship between thickness.
Liu et al. A stable isotope doping method to test the range of applicability of detailed balance Figure 2 Comparison of the equilibrium dissolution and.
John Grotzinger, Thomas H. Jordan,
John Grotzinger, Thomas H. Jordan,
T.P. Galbraith, R. Harris, P.C. Driscoll, B.A. Wallace 
John Grotzinger, Thomas H. Jordan,
Why is there melting and volcanism at subduction zones?
Michele Curcio, Frank Bradke  Neuron 
Formation of Stony-Iron Meteorites in Early Giant Impacts
Groundwater Learning objectives
Molecular hydrogen in mantle minerals
Molecular hydrogen in mantle minerals
FUS Zigzags Its Way to Cross Beta
John Grotzinger, Thomas H. Jordan,
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.
Michele Curcio, Frank Bradke  Neuron 
CHAPTER 18: VOLCANOES SECTION 1: MAGMA
Towards an Individualized Delineation of Functional Neuroanatomy
The NPC-Transporter, A Ghost in the Machine
Centroid TUTORIAL.
Schematic cross-section from the eastern Alcock Rise across the East Andaman Basin, SE offshore Myanmar. Schematic cross-section from the eastern Alcock.
Continuous Reactions.
Fig. 2 Ferroelectric domains resolved in WTe2 single crystals.
John Grotzinger, Thomas H. Jordan,
Ferric iron content of garnet and spinel from mantle rocks plotted as a function of the calculated log fO2 using equations (9)–(11). Ferric iron content.
Basal bodies Current Biology
Earthquakes track subduction fluids from slab source to mantle wedge sink by Felix Halpaap, Stéphane Rondenay, Alexander Perrin, Saskia Goes, Lars Ottemöller,
T.P. Galbraith, R. Harris, P.C. Driscoll, B.A. Wallace 
Presentation transcript:

van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a) Tauern Eclogite Zone P–T path (Zimmermann et al., 1994) with conditions recorded by tourmaline growth zones shown. Inset cartoons locate these in a schematic subduction-zone cross-section. (b) PPL image of the tourmaline transect. (c) XMg sharply defines the tourmaline growth zones. (d) F-content in tourmaline, >0.5 apfu F in the outer core and mantle. (e) XCa of tourmaline, which tracks the XCa in the coexisting fluid (von Goerne et al., 2011). (f) Temperature transect across the tourmaline grain calculated from inter-sector and inter-polar thermometry. (g) Tourmaline K-content, which acts as a qualitative barometer. Uncertainties shown are the typical 1s analytical precision. Figure 1 Reading the Tauern tourmaline record. (a) Tauern Eclogite Zone P–T path (Zimmermann et al., 1994) with conditions recorded by tourmaline growth zones shown. Inset cartoons locate these in a schematic subduction-zone cross-section. (b) PPL image of the tourmaline transect. (c) XMg sharply defines the tourmaline growth zones... van Hinsberg et al. (2017) Geochem. Persp. Let. 3, 160-169 | doi: 10.7185/geochemlet.1719 © 2017 European Association of Geochemistry

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2025 SlidePlayer.com. Inc. All rights reserved.