University of California, Riverside

Department of Earth Sciences



Harry W. Green


GreenDistinguished Professor of Geology and Geophysics


Ph.D., Univ. of California, Los Angeles, 1968

Specialty: Earthquake Physics; Ultra-High-Pressure Metamorphism; Mantle Rheology

Email: harry.green@ucr.edu
Phone: (951) 827-4508







Research Interests:

Experimental deformation of rocks and minerals at high temperature and pressure, earthquake physics, ultrahigh pressure metamorphism, rheology of the mantle, mechanisms of phase transformations, metastable phase equilibria, nonhydrostatic thermodynamics.

Recent Projects:

Laboratory: Physical mechanisms underlying intermediate- and deep-focus earthquakes; rheology of eclogite; origin of decompression microstructures in ultra-high pressure metamorphic rocks.
Field: Decompression microstructures in rocks subjected to ultra-high pressure metamorphism; growth of diamonds in metamorphic rocks; Origin and significance of Pseudotachylyte in Eclogite.
Theoretical: Disequilibrium thermodynamics; the effect of stress on polymorphic phase transformations; mechanism of growth of metamorphic diamonds; why do faults form at 30° to compression?;

Selected Publications:

Earthquake Physics

Jung H and Green II HW, 2005. Experimental faulting of serpentinite during dehydration: Implications for earthquakes, seismic low-velocity zones, and anomalous hypocenter distribution in subduction zones. International Geology Review 46:1089-1102.

Green, Harry W. II and Jung, Haemyeong (2005) Fluids, Faulting, and Flow. Elements, 1:31-37.

Green, II, H.W. 2005. New light on deep earthquakes. In Our Everchanging Earth, special edition (electronic version), pp.97-105, Scientific American, www.sciam.com

Zhang, J., H.W. Green, K.N. Bozhilov, Z-M Jin, 2004. Faulting induced by precipitation of water at grain boundaries in hot subducting oceanic crust. Nature 428:633-636.

Jung, H., H.W. Green, II, L.F. Dobrzhinetskaya 2004. Intermediate-depth earthquake faulting by dehydration embrittlement with negative volume change. Nature 428:545-549.

Green, H.W., II. 2003. Tiny triggers deep down. Nature 424:893-894. Invited News and Views.

Green, H.W., II, C.J. Marone. 2002. Instability of deformation, in Plastic Deformation of Minerals and Rocks, Wenk, H.R. and Karato S. eds., pp. 181-199, Mineral Soc. Amer., Washington, DC.

Green, H.W., II. 2001. Deep Tonga backarc: Graveyard for buoyant slabs bearing metastable olivine? Science 292:2445-2446. Invited Perspective

Green, H.W., II, and H. Houston. 1995. The mechanics of deep earthquakes. Ann. Rev. Earth and Planet. Sci., 23:169:213.

Green, H. W., II, T. E. Young, D. Walker and C. H. Scholz. 1990 Anticrack-associated faulting at very high pressure in natural olivine. Nature 348:720-722.

Burnley, P. C. and H. W. Green II. 1989 Stress dependence of the mechanism of the olivine-spinel transformation. Nature 338:753-756.

Green, H. W., II and P. C. Burnley. 1989 A new self-organizing mechanism for deep-focus earthquakes. Nature 341:733-737.


Ultra-High-Pressure Metamorphism

Dobrzhinetskaya, L.F., Wirth, R., Green II, H.W. 2005a. Direct Observation and Analysis of Trapped COH Fluid Growth Medium in Metamorphic Diamond. Terra Nova 17:472-477.

Green II HW, 2005. Psychology of a changing paradigm: 40+ years of high-pressure metamorphism. International Geology Review 47:439-456).

Green, H.W., II. 2004. Shock-Induced Minerals in Meteorite Provide Prospecting Tool for Mineral Physics. PNAS 101:6-7.

Dobrzhinetskaya LF, Renfro AP, Green II, HW 2004. Synthesis of skeletal diamonds: Implications for microdiamond formation in orogenic belts. Geology 32:869-872.

Dobrzhinetskaya LF, Green II, HW, Renfro AP, Bozhilov KN, Spengler D, van Roermund HLM. 2004. Precipitation of pyroxenes and Mg2SiO4 from majoritic garnet: Simulation of peridotite exhumation from great depth. Terra Nova 16:325-330.

Dobrzhinetskaya LF, HW Green, II, M Weshler, M Darus, Y-C Wang, H-J Massonne and B Stöckhert. 2003. Focused Ion Beam Technique and Transmission Electron Microscope Studies of Microdiamonds from the Saxonian Erzgebirge, Germany. Earth Planet. Sci. Letts., 210:399-410.

Bozhilov, K.N., L.F. Dobrzhinetskaya, and H.W. Green, II. 2003. Quantitative 3D measurement of ilmenite abundance in Alpe Arami olivine: Confirmation of high pressure origin. Am Mineral. 88:596-603.

Bozhilov, K.N., H.W. Green, II., L. Dobrzhinetskaya. 1999. Clinoenstatite in the Alpe Arami periodotite: additional evidence for very high-pressure. Science, 284:128-132.

Dobrzhinetskaya, L., H.W. Green, II, S. Wang. 1996. Alpe Arami: A peridotite massif from depths of more than 300 km. Science, 271:1841-1845 (Cover article).

Mantle Rheology

Zhang, J., H.W. Green, II. On the Deformation of UHP Eclogite: from Laboratory to Nature. Int. Geology Rev. (in press)

Jin, Z-M, J. Zhang, H.W. Green, II. and S. Jin. 2001. Eclogite rheology: implications for subducted lithosphere. Geology 29:667-670.

Jin, Z-M and H.W. Green, II. 1994. Melt topology in partially molten mantle peridotite during ductile deformation. Nature, 372:164-167 (Cover article).

 

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