Date of Degree
Access restricted until 02/23/2019
PhD (Doctor of Philosophy)
Jane A. Gilotti
First Committee Member
Charles T. Foster Jr.
Second Committee Member
Sara E. Mason
Third Committee Member
Fourth Committee Member
William C. McClelland
Fifth Committee Member
David W. Peate
Exhumation of high-pressure and ultrahigh-pressure eclogites in large orogens and associated petrological change during the process remain enigmatic problems. This dissertation examines eclogites from high-pressure (HP) and ultrahigh-pressure (UHP) terranes in the North-East Greenland Eclogite Province, aiming to decipher their metamorphic pressure-temperature (P-T) paths, evaluate spatial variation of P-T paths, and understand petrological changes during the exhumation.
Kyanite-bearing UHP eclogites from North-East Greenland contain a peak mineral assemblage of phengite, garnet, omphacite, kyanite, coesite, rutile and probably epidote-group minerals. Thermodynamic modeling with an XRF-derived bulk composition yielded a peak P-T condition of 3.4 GPa and 920 °C. Petrographic textures, such as graphic intergrowth of amphibole and plagioclase, cusps of plagioclase into garnet and quartz, and neoblasts of garnet indicate that the eclogites were partially melted through dehydration melting of phengite and epidote-group minerals. Since thermodynamic modeling could not yield a satisfactory solidus curve, experimental phase relations were considered in interpreting the melting process, and show a near isothermal decompression path across the epidote mineral melting curve. Additional thermodynamic modeling of a symplectite after omphacite, consisting of amphibole, plagioclase and clinopyroxene, yields a P-T condition of ~ 1.2 GPa and 800 °C. Thermodynamic modeling of a melt pocket yields a further P-T constraint of 1.4 GPa and 740 °C.
The HP zoisite eclogites from the Storstrømmen shear zone in the Sanddal area preserve partial melting textures both in garnet and in the matrix. The textures include multiphase solid inclusions of albite and K-feldspar in garnet, graphic intergrowth of amphibole and plagioclase, cuspate textures, and leucosome. Thermodynamic modeling combined with mineral composition and modes yielded an exhumation P-T path from subsolidus conditions at ~1.95 GPa and ~670 °C, to ~1.85 GPa and 715 °C at suprasolidus, to ~1.45 GPa and 640 °C. Paragonite, phengite, and amphibole were the major dehydration melted phases along the exhumation path.
The HP kyanite eclogite from the Danmarkshavn area contains disequilibrium textures developed during retrograde stages. Petrographic observation documents two groups of textures: a strongly zoned plagioclase (anorthite to andesine) enclosing a poorly developed symplectite of sapphirine + spinel + plagioclase after kyanite, and a less zoned plagioclase (labradorite to andesine) enclosing a fully developed symplectite after kyanite. Thermodynamic modeling of the bulk rock returns a peak P-T condition of 1.9 GPa and 840 °C. Thermodynamic modeling of a symplectite domain yields poor P-T constraints of 0.8 – 1.3 GPa and 700 – 900 °C. Modeling also indicates the plagioclase development would be richer in Ca during decompression while progressive replacement of kyanite induced the plagioclase rim to be less Ca-rich.
This study reveals that HP and UHP eclogites may experience partial melting on their exhumation path. Dehydration melting of hydrous minerals (e.g. phengite and zoisite) is the most plausible way in partially melt the eclogites, because of limited amounts of free fluid. The partial melting does not trigger exhumation of the eclogites, but may facilitate the exhumation process. The near-isothermal exhumation path for the UHP terranes suggests that it was initially exhumed through vertical extrusion. Lateral extrusion by the Storstrømmen and Germania Land shear zones is suggested to have further exhumed the HP and UHP rocks, which is analogous to the lateral escape tectonics in the Tibetan Plateau
Continental material can subduct to mantle depths (≥ 60 km) during continental collision and exhume back to the surface. These exhumed rocks preserve records probing processes at deeper parts of the Earth. This dissertation examines eclogite from North-East Greenland, where eclogites is a mafic rock, mainly composed of garnet and omphacite, metamorphosed at high pressure. The aim of this research is to estimate pressure-temperature (P-T) paths of the eclogites and to understand associated petrological changes during their exhumation. Thermodynamic modeling reveals that kyanite eclogites from Rabbit Ears Island reached a P-T condition of 3.4 GPa, 920 °C, which is at about 110 km below the surface. Minerals and mineral compositions suggest that epidote-group minerals were a major melted phase. Thermodynamic modeling of zoisite eclogites yields an exhumation P-T path from peak pressure ~1.95 GPa (~ 65 km) at ~670 °C at subsolidus conditions, to 715 °C at ~1.85 GPa (~ 61 km) at suprasolidus, and to ~1.45 GPa (~ 48 km), 640 °C. Petrographic textures and mineral compositions indicate that paragonite, phengite and amphibole were major partially melted minerals. Thermodynamic modeling of kyanite eclogites from Danmarkshavn yields a peak P-T at 1.9 GPa and 840 ˚C, indicating that the samples were at ~63 km below the surface, with poorly constrained retrograde conditions. This systematic study suggests that 1) the latter two localities were from a relatively homogeneous orogenic root, and 2) different exhumation paths may lead to melting of minerals or development of retrogressed textures depending on local bulk compositions.
Caledonides, Eclogite, North-East Greenland, Partial melting, Pressure-temperature path, Pseudosection modeling
xxii, 220 pages
Includes bibliographical references (pages 210-220).
Copyright © 2016 Wentao Cao
Cao, Wentao. "Metamorphic pressure-temperature paths of eclogites from The North-East Greenland Caledonides." PhD (Doctor of Philosophy) thesis, University of Iowa, 2016.
Available for download on Saturday, February 23, 2019