Volatile Recycling at Subduction Zones Terry Plank, Lamont Doherty Earth Observatory The Subduction Factory.

Slides:



Advertisements
Similar presentations
Earth Science 10.1 Volcanoes and Plate Tectonics
Advertisements

WHAT IS MAGMA MADE UP OF?. At divergent boundaries and hot spots, magma forms by PARTIAL MELTING (not complete melting) of the mantle Minerals with higher.
Sources of CO 2 at the Earth’s surface (and CH 4 ) MORs pockmark fields CH 4 vents Arc CO 2 (Fuego, Guatemala) Metamorphic degassing CO 2 MCT zone Nepal.
Plate Tectonics.
Lecture-10 1 Lecture #10- Subduction Zones. Lecture-10 2 Subduction Zones F When two tectonic plates converge often one will get buried or subducted beneath.
Plate Tectonics. What is Plate Tectonics? According to the plate tectonics theory, the uppermost mantle, along with the overlying crust, behaves as a.
What is the role of Subduction in Deep Earth Volatile Cycles? Marc Hirschmann University of Minnesota.
Dept. Earth SciencesJ. Huw Davies, Hydrofrac Model Davies, Nature, 1999.
Title Mariana melting and thermal structure James A. Conder Dept. of Earth and Planetary Sciences Washington University James A. Conder Dept. of Earth.
A low velocity layer (LVZ) at the top of the subducting plate has been detected in a majority of subduction zones. LVZ may be a hydrated layer of oceanic.
GEOLOGY Study of the Earth’s processes. Science that is concerned with the history of the Earth and its life, especially as recorded in rocks.
PLATE TECTONICS.
The Tonga-Kermadec arc – Lau back-arc: recent progress and future directions Simon Turner.
Volcanoes and Plate Tectonics
Lecture 3: Earth's Structure, Plate Tectonics, and the Rock Cycle Our Hazardous Environment GEOG 1110 Dr. Thieme.
Climate Systems Chapter 15. Clicker Question What is the approximate CO 2 content of the atmosphere? –A % (40 ppm) –B. 0.04% (400 ppm) –C. 0.4%
Sedimentary input to the source of Lesser Antilles lavas: A Li perspective Ming Tang 1, Roberta Rudnick 1, Catherine Chauvel 2 1.Department of Geology,
Melting Regions of the Mantle Terry Plank: LDEO with C-T. Lee (Rice) D. Forsyth (Brown) E. Hauri (Carnegie ) K.Fischer (Brown) G. Abers (LDEO) D.Wiens.
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.
Basic research needs workshop for Materials Under Extreme Environments Plenary Closing Session June 13, 2007 BREAKOUT SESSION 2: DEEP CARBON FLUXES What.
Sea Floor Spreading & Plate Tectonics Ch.2 The Sea Floor.
What can (and cannot) be learned from scientific drilling
The process that creates and changes rocks
Get out: Earthquake notes 5-2 Homework. Volcanoes and Plate Tectonics Section 9-2.
The Ongoing and the Early Differentiation of the Earth: the Role of Volatiles Rajdeep Dasgupta June 26, 2008COMPRES.
IBM’s Second Arc Jim Gill, UCSC SubFac has transformative potential... But beware of consensus: Some of what Rummie said he knew wasn’t true.
How are oceans formed? Continents and ocean basins exist on lithospheric plates that move relative to each Other. Between their margins, new land is always.
Melting processes and volatile fluxes at the Gakkel Ridge – do ultra-slow spreading systems reveal insights to Rift evolution? Alison Shaw, Mark Behn,
Oceanic Spreading Centers. Structure of a fast spreading center (East Pacific Rise ~ 10 cm/yr)
Volatile fluxes at arc volcanoes: comparing different techniques and evaluating mass balance A. Shaw, D. Hilton, T. Fischer, E. Hauri Arenal Volcano.
Volcanos: Chapter Volcano A volcano is a week spot in the crust where molten material, or magma, comes to the surface.
Plate Tectonics: Boundaries!
Earth’s Deep Volatile Cycles Hydrogen Carbon (diagram courtesy of J Phipps-Morgan)
Glenn Spinelli Effects of fluid circulation in ocean crust on subduction zone temperatures and metamorphism.
Plate Boundaries. Convergent Boundaries 2 plates move toward each other Destructive plate margins Old plate material is being recycled Oceanic crust.
Carbon Cycling in Subduction Zones implications for mantle-exosphere exchange Rajdeep Dasgupta.
An Izu-Bonin-Mariana Arc Thematic Mini-Lesson Package. Initiated by Jeff Ryan (University of South Florida), Rosemary Hickey-Vargas (Florida International.
Seismogenic Characteristics and Seismic Structure of the Mariana Arc: Comparison with Central America Douglas A. Wiens, James Conder, Sara Pozgay, Mitchell.
VOLCANOES & IGNEOUS ACTIVITY CHAPTER 10. Section 10.1.
Volcanoes and Plate Tectonics Chapter 6 Section 1.
9.3 Actions at Plate Boundaries
Continental Drift and Plate Tectonics (notes pt. 2)
Non-Traditional Isotope Laboratory
Island Arc Magmatism Eruption of Anatahan Volcano,
Theory of Plate Tectonics
Warm Up 11/3 What hypothesis states that the continents were once joined to form a single supercontinent? a. continental drift c. plate tectonics b.
Plate Tectonics.
Squeezing the Slab: future directions for metamorphic petrology in the SZO Andrew Smye Sentence about metamorphic petrology and need to link observations.
Ocean-Ocean Subduction Zones System
PLATES AND TECTONIC MOVEMENT
Plate boundaries & convection currents
Plate Boundaries Convergent plate boundaries (destructive margins)
Notes on Plate Tectonics
ACTIONS AT PLATE BOUNDARIES
SUBDUCTION AND PLATE TECTONICS
Theory of Plate Tectonics (1960) Earth’s lithosphere consists of rigid, but moving masses called tectonic plates.
Notes on Plate Tectonics
MARGINS Subduction Factory.
9.3 – Actions at Plate Boundaries – Part II
9.3 Actions at Plate Boundaries
Structure of the Earth.
Volcanoes.
9.3 Actions at Plate Boundaries
9.3 Actions at Plate Boundaries
ACTIONS AT PLATE BOUNDARIES
CHAPTER 18: VOLCANOES SECTION 1: MAGMA
Plate Tectonics Part II: Plate Boundaries.
Aim: How do the plates of the Earth move?
INSIDE EARTH: CHAPTER 3- VOLCANOES
9.3 Actions at Plate Boundaries
Presentation transcript:

Volatile Recycling at Subduction Zones Terry Plank, Lamont Doherty Earth Observatory The Subduction Factory

Is the Ocean Shrinking?

60% of structurally- bound H 2 O released Hacker (2008) G3; Jarrard (2003) G3 Water Fluxes During Subduction

60% of structurally- bound H 2 O released Hacker (2008) G3 Water Fluxes During SubductionH 2 O Output? H 2 O % in magma Magma Mass Flux

Centam H 2 O (least degassed) wt% Arc Data: 2000 MORBMORB (SubFac Science Plan)

Aleutians Centam Marianas Mexico Tonga Kamchatka H 2 O (least degassed) wt% Arc Data: 2009 MORBMORB 3.9 wt% H 2 O +/- 1.0 (1 stdev)

Average Arc Growth Rates Suyehiro et al. (1996) Science Holbrook et al (1999) Geology ( km 3 /km/Ma) Izu Arc Aleutian Arc (Reymer&Schubert, 1984) (Holbrook et al., 1999) (Dimalanta et al., 2002) (Jicha et al., 2006) Duration: 46 Ma 28 (Reymer&Schubert, 1984) 66 (Suyehiro et al., 1996) (Dimalanta et al., 2002) Duration: 47 Ma

Th input (g/yr) Th output (g/yr) = C Th * Magma Mass Flux Hebert et al (2009) 100 km

60% of structurally- bound H 2 O released Hacker (2008) G3 Water Fluxes During Subduction4 +/- 1 wt% H 2 O arcs 60 +/- 20 km 3 /km/Ma 3.0E8 = 40 +/- 20 % recycled to arc

Millions of years before present Relative sea level change (meters) 70% 40% 50% Subduction of Water Lowering Sea Level 50% water recycled to surface from Rupke et al. (2004)

Millions of years before Present Global Sea Level Variations meters Hallam (1982); and Wallman (2001) Sea level fall over past ~ 600 Ma due to subduction of water??

from Rupke et al, Earth and Planetary Science Letters (2004) Size of Ocean today Ocean growing Ocean shrinking hotter mantle cooler mantle

2% H 2 O in 4 km mantle 5.7

All serpentine- bound H 2 O bypasses arc? Hacker (2008) G3 Water Fluxes During Subduction

2% H 2 O in 4 km mantle 5.7 past arc Lose ocean In 1.7 Ga!

Wiens/Lizarralde MARGINS experiment

Subducting Carbonate and CO 2 Cycling

GLOSS - global subducting sediment Plank & Langmuir (1998) Centam Plank, et al (2002) Geology

Altered oceanic crust Alt figure?? (1999) GCA

CO 2 Output?? Figure from Wallace (2005) JVGR

Melt Inclusions - minimum CO 2 ? Benjamin et al. (2007) JVGR -- Irazu Volcano, Costa Rica

Global Flux Estimates from Wallace (2005) JVGR

C Flux in & out of the mantle (Alt & Teagle, 1999; Sleep & Zahnle, 2001; Jarrard, 2003) Courtesy of M. Hirschmann Input Output 25%

Centam, CO 2 flux from slab Gorman et al (2006) G3

Shaw et al (2003) EPSL Typical CO 2 / 3 He in Centam despite major carbonate subduction

H 2 O Recycling REE/Th CO 2 Recycling 40-60% returned to arc serpentine subduction? 25% returned to arc decarbonation? CO 2 fluxes out volcanoes