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The Magmatic Architecture of Continental Flood Basalts I: Observations From the Deccan Traps
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Abstract
Flood basalts are some of the largest magmatic events in Earth history, with intrusion and eruption of millions of km 3 of basaltic magma over a short time period (∼1–5 Ma). A typical continental flood basalt (CFB) is emplaced in hundreds of individual eruptive episodes lasting decades to centuries with lava flow volumes of 10 3 –10 4 km 3 . These large volumes have logically led to CFB models invoking large magma reservoirs ( –10 5 km 3 ) within the crust or at Moho depth. Since there are currently no active CFB provinces, we must rely on observations of past CFBs with varying degrees of surface exposure to develop and test models. In the last few decades, significant improvements in geochronological, geochemical, paleomagnetic, volcanological, and paleo‐proxy measurements have provided high‐resolution constraints on CFB eruptive tempo ‐ the volume, duration, and frequency of individual eruptive episodes. Using the well‐studied Deccan Traps as an archetype for CFB systems, we compile multiple lines of evidence–geochronology, eruption tempo, dike spatial distribution, intrusive‐extrusive ratio, geochemical variations, and volcanological observations–to assess the viability of previous models. We find that the presence of just a few large crustal magma reservoirs is inconsistent with these constraints. Although observations from the Deccan Traps primarily motivate our model, we discuss constraints from other CFBs to illustrate that this conclusion may be broadly applicable for CFB magmatic systems in general.
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Mittal, T., & Richards, M. A. (2021) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2021jb021807 · Cited by 16
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Metadata
- Authors
- Mittal, T., Richards, M. A., & Fendley, I. M.
- Affiliations
- Massachusetts Institute of Technology (US)
- University of Washington (US)
- University of Oxford (GB)
- Corresponding author
- Mittal, Tushar
- Venue
- Journal of Geophysical Research: Solid Earth
- Publisher
- American Geophysical Union (AGU)
- Published
- 2021-12
- Volume
- 126
- Issue
- 12
- ISSN
- 2169-9313 (ISSN-L)
- 2169-9356
- OpenAlex
- W3126930214
- Cited by
- 42
- References
- 429
- Citations by year
- 2026: 4 · 2025: 14 · 2024: 7 · 2023: 10 · 2022: 5 · 2021: 2
- FWCI
- 3.22
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Licence
- Locations
- Journal of Geophysical Research Solid Earth (publishedVersion, cc-by-nc)
- DSpace@MIT (Massachusetts Institute of Technology) (submittedVersion, cc-by-nc)
- Funders
- National Science Foundation (1615203)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- continental flood basalts, Deccan Traps, magma chamber, basalt geochemistry, geochronology, crustal magma storage
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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