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(Appendix B) Magnetic polarity, inclination angle, and maximum angular deviat...
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Regional benthic δ¹⁸O stacks and their δ¹⁸O uncertainties
Benthic δ18O changes are often assumed to be globally synchronous, but studies comparing 2–9 radiocarbon‐dated records over the most recent deglaciation (Termination 1) have... -
(Table 1) Paleomagnetic of reoriented core pieces of IODP Hole 304-U1309D
Oceanic core complexes expose lower crustal and upper mantle rocks on the seafloor by tectonic unroofing in the footwalls of large-slip detachment faults. The common occurrence...
