Journal of Geophysical Research: Solid Earth
The presence of calcite as the dominant carbonate mineral, and similar δ 13 C, δ 18 O, and 87 Sr/ 86 Sr signatures are further evidence for a genetic relationship with the overlying limestone units, which were deposited from Late Cretaceous to Paleogene (de Obeso & Kelemen, 2018; Schlüter et al., 2008). Here we use (U-Th)/He chronometry …