Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/118285
Citations
Scopus Web of Science® Altmetric
?
?
Type: Journal article
Title: Nanoscale study of lamellar exsolutions in clinopyroxene from olivine gabbro: recording crystallization sequences in iron-rich layered intrusions
Author: Gao, W.
Ciobanu, C.
Cook, N.
Slattery, A.
Huang, F.
Wang, D.
Citation: American Mineralogist, 2019; 104(2):244-261
Publisher: Mineralogical Society of America
Issue Date: 2019
ISSN: 0003-004X
1945-3027
Statement of
Responsibility: 
Wenyuan Gao, Cristiana L. Ciobanu, Nigel J. Cook, Ashley Slattery, Fei Huang, and Daoheng Wang
Abstract: Pyroxene exsolutions and associated Fe–Ti oxides and spinels are described in a sample of olivine gabbro representing the Middle Zone of the Panzhihua layered intrusion, Southwest China, part of the Emeishan LIP. High-angle annular dark-field scanning transmission electron microscope imaging, electron diffraction, and energy dispersive spectroscopy reveal complex multi-stage exsolution relationships in the host clinopyroxene. The studied assemblage is common in gabbroic rocks and comprises subcalcic diopside and lamellar clinoenstatite (<1 wt% Ca). Two sets of exsolved clinopyroxene lamellae are observed. Only one is, however, well developed as lamellae oriented approximately parallel to (801) of diopside, making an angle of ~10 to 11° with the (100) planes, or the c axis, of both phases. These are the so-called “100” lamellae with a perfect fit along a-crystallographic axes when viewed down to [010] zone axis. Crosscutting exsolutions of Fe–(Ti) oxides are relatively common throughout the same host clinopyroxene. Apart from ilmenite and magnetite with variable Ti-content, hercynite is a minor yet ubiquitous phase. The nanoscale study indicates a sequence of fine-scale processes: from higher-T (~1030–1100 °C): (I) (clino)enstatite exsolutions in low-Ca diopside; followed by (II) slightly Ca-richer diopside overgrowths and high-T titanomagnetite exsolution in diopside; to lower-T (<450 °C) (III) titanomagnetite exsolutions into ulvöspinel + magnetite; followed by (IV) sub-solidus re-equilibration in clinopyroxenes and among Fe–Ti oxides + hercynite. Using exact phase boundary theory, pressures of lamellar exsolution within the host diopside are estimated as ~2 GPa with an error of ± ≤1 GPa. The present study of complex exsolutions in clinopyroxene demonstrates that a nanoscale approach can help constrain P-T-X evolution during formation of layered intrusions.
Keywords: High-angle annular dark-field scanning transmission electron microscopy; clinopyroxene; titanomagnetite; liquid-magmatic ore deposits; sequence of exsolution
Rights: © 2019 by the Mineralogical Society of America
RMID: 0030108886
DOI: 10.2138/am-2019-6764
Appears in Collections:Chemical Engineering publications

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.