The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada

Deposited with permission of the author. © 1996 Derek Christian Vogel. The Early Proterozoic Agnew Intrusion is a well-preserved leucogabbronoritic to gabbronoritic layered intrusion that is a member of the East Bull Lake suite of layered intrusions (ca. 2490-2470 Ma) occurring in central Ontario. T...

Full description

Bibliographic Details
Main Author: Vogel, Derek Christian
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: 2004
Subjects:
Agnew Intrusion
petrogenesis
intrusion
Huronian
Ontario
Canada
geology
geochemistry
Bull Lake
Fennoscandian
Online Access:http://hdl.handle.net/11343/39455
id ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/39455
record_format openpolar
spelling ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/39455 2023-05-15T16:12:57+02:00 The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada Vogel, Derek Christian 2004-12-09 http://hdl.handle.net/11343/39455 unknown Vogel, D. C. (1996). The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada. PhD thesis, School of Earth Sciences, The University of Melbourne. http://hdl.handle.net/11343/39455 Terms and Conditions: Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works. Agnew Intrusion petrogenesis intrusion Huronian Ontario Canada geology geochemistry PhD thesis 2004 ftumelbourne 2019-10-15T12:09:33Z Deposited with permission of the author. © 1996 Derek Christian Vogel. The Early Proterozoic Agnew Intrusion is a well-preserved leucogabbronoritic to gabbronoritic layered intrusion that is a member of the East Bull Lake suite of layered intrusions (ca. 2490-2470 Ma) occurring in central Ontario. These intrusions are related to the development of the Huronian Rift Zone, which may be part of a much more widespread rifting event that involved the Fennoscandian Shield. Structural data suggest that these intrusions have been subjected to ductile deformation and are erosional remnants of one or more sill-like bodies originally emplaced along the contact between Archaean granitic rocks of the Superior Province and an Early Proterozoic Huronian continental flood basalt sequence in the Southern Province. Doctoral or Postdoctoral Thesis Fennoscandian The University of Melbourne: Digital Repository Bull Lake ENVELOPE(161.700,161.700,-77.533,-77.533) Canada
institution Open Polar
collection The University of Melbourne: Digital Repository
op_collection_id ftumelbourne
language unknown
topic Agnew Intrusion
petrogenesis
intrusion
Huronian
Ontario
Canada
geology
geochemistry
spellingShingle Agnew Intrusion
petrogenesis
intrusion
Huronian
Ontario
Canada
geology
geochemistry
Vogel, Derek Christian
The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
topic_facet Agnew Intrusion
petrogenesis
intrusion
Huronian
Ontario
Canada
geology
geochemistry
description Deposited with permission of the author. © 1996 Derek Christian Vogel. The Early Proterozoic Agnew Intrusion is a well-preserved leucogabbronoritic to gabbronoritic layered intrusion that is a member of the East Bull Lake suite of layered intrusions (ca. 2490-2470 Ma) occurring in central Ontario. These intrusions are related to the development of the Huronian Rift Zone, which may be part of a much more widespread rifting event that involved the Fennoscandian Shield. Structural data suggest that these intrusions have been subjected to ductile deformation and are erosional remnants of one or more sill-like bodies originally emplaced along the contact between Archaean granitic rocks of the Superior Province and an Early Proterozoic Huronian continental flood basalt sequence in the Southern Province.
format Doctoral or Postdoctoral Thesis
author Vogel, Derek Christian
author_facet Vogel, Derek Christian
author_sort Vogel, Derek Christian
title The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
title_short The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
title_full The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
title_fullStr The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
title_full_unstemmed The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada
title_sort geology and geochemistry of the agnew intrusion: implications for the petrogenesis of early huronian mafic igneous rocks in central ontario, canada
publishDate 2004
url http://hdl.handle.net/11343/39455
long_lat ENVELOPE(161.700,161.700,-77.533,-77.533)
geographic Bull Lake
Canada
geographic_facet Bull Lake
Canada
genre Fennoscandian
genre_facet Fennoscandian
op_relation Vogel, D. C. (1996). The geology and geochemistry of the Agnew Intrusion: implications for the petrogenesis of early Huronian mafic igneous rocks in Central Ontario, Canada. PhD thesis, School of Earth Sciences, The University of Melbourne.
http://hdl.handle.net/11343/39455
op_rights Terms and Conditions: Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works.
_version_ 1765998556795109376

Similar Items