| DOI: | 10.1016/j.epsl.2019.115840
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| 论文题名: | Extricating dynamic topography from subsidence patterns: Examples from Eastern North America's passive margin |
| 作者: | Morris M.; Fernandes V.M.; Roberts G.G.
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| 刊名: | Earth and Planetary Science Letters
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| ISSN: | 0012821X
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| 出版年: | 2020
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| 卷: | 530 | | 语种: | 英语
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| 中文关键词: | eustasy
; mantle convection
; Neogene
; New Jersey margin
; sea level
; subsidence
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| 英文关键词: | Geodynamics
; Geophysical prospecting
; Sea level
; Seismic response
; Seismic waves
; Shear flow
; Shear waves
; Strain rate
; Stratigraphy
; Structural geology
; Topography
; Water levels
; Dynamic topography
; Eastern north america
; Eustasy
; Geophysical observations
; Mantle convection
; Neo genes
; New Jersey
; Shear wave velocity
; Subsidence
; eustacy
; mantle convection
; Neogene
; passive margin
; S-wave
; sea level
; subsidence
; tectonic evolution
; tectonic setting
; topography
; Atlantic Ocean
; Baltimore Canyon
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| 英文摘要: | Global sea-level (eustatic) histories generated by backstripping stratigraphy are predicated upon the lithosphere having a well understood tectonic history. However, sub-plate processes play a role in governing lithospheric vertical motions with timescales and amplitudes akin to eustasy, which are difficult to predict. We examine how stratigraphic and geophysical observations combined with simple isostatic models can be used to disentangle histories of sub-plate support and eustasy. We focus on the passive margin of Eastern North America, where a generally accepted history of eustasy has been estimated. Negative long wavelength free-air gravity anomalies, residual ocean-age depth estimates, fast upper mantle shear wave velocities, and geodynamic models suggest that Cenozoic evolution of this passive margin has been influenced by upper mantle drawdown. We build on existing analyses to backstrip sixteen wells, which, combined with seismic data, constrain timing and extent of Cenozoic subsidence. Results indicate up to ∼1000 m of water-loaded subsidence between ∼20–0 Ma centered on the Baltimore Canyon Trough. Seismic data from the trough shows Neogene aggrading clinoforms. There is little evidence for faulting or stratigraphic growth, which indicates that Neogene lithospheric strain rates were low. Amplitude and spatial extent of Neogene subsidence are difficult to explain by glacio-eustasy or glacio-isostatic adjustment. Instead, sub-plate support calculated from conversion of shear wave velocities to temperature and isostatic calculations indicate that upper mantle drawdown was responsible for subsidence of the margin. Because mantle convection is vigorous such observations are expected throughout the stratigraphic archive. © 2019 |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/165176
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| Appears in Collections: | 气候变化与战略
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作者单位: | Department of Earth Science and Engineering, Imperial College London, South Kensington CampusSW7 2AZ, United Kingdom
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| Recommended Citation: | |
Morris M.,Fernandes V.M.,Roberts G.G.. Extricating dynamic topography from subsidence patterns: Examples from Eastern North America's passive margin[J]. Earth and Planetary Science Letters,2020-01-01,530
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