File Download
There are no files associated with this item.
Links for fulltext
(May Require Subscription)
- Publisher Website: 10.1002/gj.2962
- Scopus: eid_2-s2.0-85042200933
- WOS: WOS:000437675500010
- Find via
Supplementary
- Citations:
- Appears in Collections:
Article: Interplay of tectonism and eustasy during the Early Permian icehouse: Southern Sydney Basin, southeast Australia
Title | Interplay of tectonism and eustasy during the Early Permian icehouse: Southern Sydney Basin, southeast Australia |
---|---|
Authors | |
Editors | Editor(s):Tyrrell, S |
Keywords | glacio-eustasy icehouse periods Permian sequence stratigraphy southern Sydney Basin |
Issue Date | 2018 |
Publisher | John Wiley & Sons Ltd. The Journal's web site is located at http://www3.interscience.wiley.com/cgi-bin/jhome/1903 |
Citation | Geological Journal, 2018, v. 53 n. 4, p. 1372-1403 How to Cite? |
Abstract | This investigation presents an outcrop-based integrated study of sedimentological analysis and sequence stratigraphy applied to the Lower Permian sedimentary succession in the southern Sydney Basin, Australia. This succession accumulated in several depositional environments and sub-environments that range from non-marine (fluvial) to marine (outer shelf), representing the fill of a sedimentary basin that resembles a fault-bounded, rift basin. The stratigraphic analysis indicates a deepening-upward trend, and the sequence stratigraphic approach has established that these sediments can be attributed to the lowstand, transgressive, and highstand systems tracts. Lowstand sediments can be defined by fluvial facies that are located between the subaerial unconformity and the maximum regressive surface. Transgressive facies correspond to estuarine, upper and lower shoreface, and inner and outer shelf depositional environments and are located between the maximum regressive and the maximum flooding surfaces. Highstand bottomset sediments are accumulated above the maximum flooding surface and are represented by outer shelf facies. The stratigraphic architecture indicates the development of an almost complete depositional sequence, mainly developed under the control of tectonically induced subsidence, but also influenced by the high sedimentation rates and the high gradient of the inherited topography. Eustatic sea-level fluctuations were of minor importance during the deposition of the examined sediments. |
Persistent Identifier | http://hdl.handle.net/10722/308666 |
ISSN | 2023 Impact Factor: 1.4 2023 SCImago Journal Rankings: 0.530 |
ISI Accession Number ID |
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Maravelis, AG | - |
dc.contributor.author | Catuneanu, O | - |
dc.contributor.author | NORDSVAN, A | - |
dc.contributor.author | Landenberger, B | - |
dc.contributor.author | Zelilidis, A | - |
dc.contributor.editor | Tyrrell, S | - |
dc.date.accessioned | 2021-12-06T06:35:23Z | - |
dc.date.available | 2021-12-06T06:35:23Z | - |
dc.date.issued | 2018 | - |
dc.identifier.citation | Geological Journal, 2018, v. 53 n. 4, p. 1372-1403 | - |
dc.identifier.issn | 0072-1050 | - |
dc.identifier.uri | http://hdl.handle.net/10722/308666 | - |
dc.description.abstract | This investigation presents an outcrop-based integrated study of sedimentological analysis and sequence stratigraphy applied to the Lower Permian sedimentary succession in the southern Sydney Basin, Australia. This succession accumulated in several depositional environments and sub-environments that range from non-marine (fluvial) to marine (outer shelf), representing the fill of a sedimentary basin that resembles a fault-bounded, rift basin. The stratigraphic analysis indicates a deepening-upward trend, and the sequence stratigraphic approach has established that these sediments can be attributed to the lowstand, transgressive, and highstand systems tracts. Lowstand sediments can be defined by fluvial facies that are located between the subaerial unconformity and the maximum regressive surface. Transgressive facies correspond to estuarine, upper and lower shoreface, and inner and outer shelf depositional environments and are located between the maximum regressive and the maximum flooding surfaces. Highstand bottomset sediments are accumulated above the maximum flooding surface and are represented by outer shelf facies. The stratigraphic architecture indicates the development of an almost complete depositional sequence, mainly developed under the control of tectonically induced subsidence, but also influenced by the high sedimentation rates and the high gradient of the inherited topography. Eustatic sea-level fluctuations were of minor importance during the deposition of the examined sediments. | - |
dc.language | eng | - |
dc.publisher | John Wiley & Sons Ltd. The Journal's web site is located at http://www3.interscience.wiley.com/cgi-bin/jhome/1903 | - |
dc.relation.ispartof | Geological Journal | - |
dc.rights | Submitted (preprint) Version This is the pre-peer reviewed version of the following article: [FULL CITE], which has been published in final form at [Link to final article using the DOI]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. Accepted (peer-reviewed) Version This is the peer reviewed version of the following article: [FULL CITE], which has been published in final form at [Link to final article using the DOI]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. | - |
dc.subject | glacio-eustasy | - |
dc.subject | icehouse periods | - |
dc.subject | Permian | - |
dc.subject | sequence stratigraphy | - |
dc.subject | southern Sydney Basin | - |
dc.title | Interplay of tectonism and eustasy during the Early Permian icehouse: Southern Sydney Basin, southeast Australia | - |
dc.type | Article | - |
dc.identifier.email | NORDSVAN, A: nordsvan@hku.hk | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.1002/gj.2962 | - |
dc.identifier.scopus | eid_2-s2.0-85042200933 | - |
dc.identifier.hkuros | 330555 | - |
dc.identifier.volume | 53 | - |
dc.identifier.issue | 4 | - |
dc.identifier.spage | 1372 | - |
dc.identifier.epage | 1403 | - |
dc.identifier.isi | WOS:000437675500010 | - |
dc.publisher.place | United Kingdom | - |