THE CHARACTER OF THE FIELD DURING GEOMAGNETIC REVERSALS

Scott W. Bogue, Ronald T. Merrill

Annual Review of Earth and Planetary Sciences · 1992 · 53 citations · 43 references

Concepts

Abstract

Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-rich parental melts that are mostly mantle derived. They dominantly consist of carbonate minerals such as calcite, dolomite, and ankerite, as well as minor ...Read More

References

43