| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Deep Carbon and the Life Cycle of Large Igneous Provinces |
|---|
| Journal | Elements |
|---|
| Authors | Black, Benjamin A. | Author |
|---|
| Gibson, Sally A. | Author |
| Year | 2019 (October 1) | Volume | 15 |
|---|
| Issue | 5 |
|---|
| Publisher | Mineralogical Society of America |
|---|
| DOI | doi:10.2138/gselements.15.5.319Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 409579 | Long-form Identifier | mindat:1:5:409579:2 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Black, Benjamin A., Gibson, Sally A. (2019) Deep Carbon and the Life Cycle of Large Igneous Provinces. Elements, 15 (5) 319-324 doi:10.2138/gselements.15.5.319 |
|---|
| Plain Text | Black, Benjamin A., Gibson, Sally A. (2019) Deep Carbon and the Life Cycle of Large Igneous Provinces. Elements, 15 (5) 319-324 doi:10.2138/gselements.15.5.319 |
|---|
| In | (2019, October) Elements Vol. 15 (5) Mineralogical Society of America |
|---|
| Abstract/Notes | Carbon is central to the formation and environmental impact of large igneous provinces (LIPs). These vast magmatic events occur over geologically short timescales and include voluminous flood basalts, along with silicic and low-volume alkaline magmas. Surface outgassing of CO2 from flood basalts may average up to 3,000 Mt per year during LIP emplacement and is subsidized by fractionating magmas deep in the crust. The large quantities of carbon mobilized in LIPs may be sourced from the convecting mantle, lithospheric mantle and crust. The relative significance of each potential carbon source is poorly known and probably varies between LIPs. Because LIPs draw on mantle reservoirs typically untapped during plate boundary magmatism, they are integral to Earth's long-term carbon cycle. |
|---|
These are possibly similar items as determined by title/reference text matching only.
