Continent-scale Hiatus Maps for the Atlantic Realm and Australia since the Upper Jurassic and links to mantle flow induced dynamic topography
Interregional geological maps hold important information for geodynamic models. Here, we use such maps to visualize major conformable and unconformable contacts at interregional scales and at the level of geologic series from the Upper Jurassic onward across North and South America, Europe, Africa a...
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| Published in | Proceedings of the Royal Society. A, Mathematical, physical, and engineering sciences Vol. 476; no. 2242; pp. 1 - 21 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Royal Society
01.10.2020
The Royal Society Publishing |
| Online Access | Get full text |
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| Abstract | Interregional geological maps hold important information for geodynamic models. Here, we use such maps to visualize major conformable and unconformable contacts at interregional scales and at the level of geologic series from the Upper Jurassic onward across North and South America, Europe, Africa and Australia. We extract hiatus information from these paleogeological maps, which we plot in a paleogeographical reference frame to link the maps to the plate and plume modes of mantle convection. We assume that interregional patterns of hiatus surfaces are proxy records of continent-scale mantle-induced vertical motion of the lithosphere. We find significant differences in the distribution of hiatus across and between continents at the timescale of geologic series, that is ten to a few tens of millions of years (Myrs). This is smaller than the mantle transit time, which, as the timescale of convection, is about 100–200 Myrs. Our results imply that different timescales for convection and topography in convective support must be an integral component of time-dependent geodynamic Earth models, consistent with the presence of a weaker upper mantle relative to the lower mantle. Additional geological constraints together with interregional geological maps at the resolution of stages (1–2 Myrs), are needed to assist in future geodynamic interpretations of interregional geologic hiatus. |
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| AbstractList | Interregional geological maps hold important information for geodynamic models. Here, we use such maps to visualize major conformable and unconformable contacts at interregional scales and at the level of geologic series from the Upper Jurassic onward across North and South America, Europe, Africa and Australia. We extract hiatus information from these paleogeological maps, which we plot in a paleogeographical reference frame to link the maps to the plate and plume modes of mantle convection. We assume that interregional patterns of hiatus surfaces are proxy records of continent-scale mantle-induced vertical motion of the lithosphere. We find significant differences in the distribution of hiatus across and between continents at the timescale of geologic series, that is ten to a few tens of millions of years (Myrs). This is smaller than the mantle transit time, which, as the timescale of convection, is about 100–200 Myrs. Our results imply that different timescales for convection and topography in convective support must be an integral component of time-dependent geodynamic Earth models, consistent with the presence of a weaker upper mantle relative to the lower mantle. Additional geological constraints together with interregional geological maps at the resolution of stages (1–2 Myrs), are needed to assist in future geodynamic interpretations of interregional geologic hiatus. |
| Author | Vibe, Yulia Carena, Sara Bunge, Hans-Peter Friedrich, Anke M. Hayek, Jorge Nicolas Vilacís, Berta |
| AuthorAffiliation | Ludwig-Maximilians-Universität München , Department of Earth and Environmental Sciences , Theresienstraße 41 and Luisenstraße 37, 80333 Munich , Germany |
| AuthorAffiliation_xml | – name: Ludwig-Maximilians-Universität München , Department of Earth and Environmental Sciences , Theresienstraße 41 and Luisenstraße 37, 80333 Munich , Germany |
| Author_xml | – sequence: 1 givenname: Jorge Nicolas surname: Hayek fullname: Hayek, Jorge Nicolas – sequence: 2 givenname: Berta surname: Vilacís fullname: Vilacís, Berta – sequence: 3 givenname: Hans-Peter surname: Bunge fullname: Bunge, Hans-Peter – sequence: 4 givenname: Anke M. surname: Friedrich fullname: Friedrich, Anke M. – sequence: 5 givenname: Sara surname: Carena fullname: Carena, Sara – sequence: 6 givenname: Yulia surname: Vibe fullname: Vibe, Yulia |
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| Title | Continent-scale Hiatus Maps for the Atlantic Realm and Australia since the Upper Jurassic and links to mantle flow induced dynamic topography |
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