(Q56059842)
Statements
Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene (English)
0 references
December 1995
0 references
10
0 references
6
0 references
965-971
0 references
1 reference
1 reference
1 reference
1 reference
1 reference
1 reference
1 reference