EventsThe 4th International Electronic Conference on Geosciences
Published
This submission belongs to the session c. Sedimentology, Stratigraphy and Palaeontology of the event The 4th International Electronic Conference on Geosciences
Published date
09 Jan, 2023
Academic Editor
author-avatarAngelos G. Maravelis
Citation
Eun Young Lee, Maria Luisa Garcia Tejada, Bernhard Schnetger, Hans-Jürgen Brumsack, Laurent Riquier, Lloyd T. White, Seung Soo Chun, Petrophysical characteristics of hydrothermally altered volcaniclastic-rich sedimentary rocks on the Naturaliste Plateau, offshore southwestern Australia (IODP Site U1513), in Proceedings of The 4th International Electronic Conference on Geosciences, 1 December–15 December 2022, MDPI: Basel, Switzerland, doi: 10.3390/IECG2022-13955
Share
Email
Facebook
Twitter
LinkedIn

Petrophysical characteristics of hydrothermally altered volcaniclastic-rich sedimentary rocks on the Naturaliste Plateau, offshore southwestern Australia (IODP Site U1513)

image
Laurent Riquier 2
Maria Luisa Garcia Tejada 3
Seung Soo Chun 4
Bernhard Schnetger 6
Hans-Jürgen Brumsack 6
1. Department of Geology, University of Vienna, 1090 Vienna, Austria, Austria
2. Institut des Sciences de la Terre de Paris (ISTeP), Sorbonne University, 75005 Paris, France,
3. Institute for Marine Geodynamics (IMG), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Kanagawa, 237-0061, Japan
4. Faculty of Earth Systems and Environmental Sciences, Chonnam National University, Gwangju 61186, Republic of Korea
5. GeoQuEST Research Centre, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, NSW 2522, Australia
6. Institute for Chemistry and Biology of the Marine Environment (ICBM), University of Oldenburg, 26129 Oldenburg, Germany
Abstract

Drilling at Site U1513 recovered the Lower Cretaceous volcaniclastic-rich sedimentary sequence on the Naturaliste Plateau and Mentelle Basin, offshore southwestern Australia. The sequence exhibits distinct lithologic characteristics, attributed to volcanism and subsidence occurred during the breakup between Greater India and Australia-Antarctica. It consists of sandstones, siltstones, and silty claystones with abundant volcanic clasts, lithics, and hydrothermal alteration. This study characterizes petrophysical properties of the sequence and correlate them with lithologic and mineralogical features. The properties show noticeable variations. Our results confirm that the petrophysical characteristics are associated with grain size, volcanic matter, organic content, as well as hydrothermal alteration minerals.

Keywords
volcaniclastic-rich sequence
IODP Site U1513
petrophysical properties
hydrothermal alteration
calcite cementation
Naturaliste Plateau
Mentelle Basin
southwest Australia
East Gondwana breakup
Early Cretaceous
Manuscript
Line of sight glacier velocity estimation of transboundary glaciers in Eastern Himalayas using high-resolution TerraSAR-X data.
The Four Principal Megabiases in the Known Fossil Record: Taphonomy, Rock Preservation, Fossil Discovery and Fossil Study