Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang, YK Chen-Wiegart… - Proceedings of the …, 2015 - National Acad Sciences
The Paleocene–Eocene boundary (∼ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …

[PDF][PDF] Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wanga, J Wangb, YK Chen-Wiegartb, DV Kentc - eps.rutgers.edu
Results In this study, we used a recently developed full-field hard X-ray ultrahigh-resolution
(∼ 30–50 nm without binning pixels) synchrotron-based transmission X-ray microscope …

Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang, YK Chen-Wiegart, DV Kent - 2015 - academiccommons.columbia.edu
Results In this study, we used a recently developed full-field hard X-ray ultrahigh-resolution
(∼ 30–50 nm without binning pixels) synchrotron-based transmission X-ray microscope …

[引用][C] Quantified abundance of magnetofossils at the Paleocene-Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang… - … of the National …, 2015 - scholarship.libraries.rutgers.edu

Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang, YK Chen-Wiegart, DV Kent - Proceedings of the National …, 2015 - JSTOR
The Paleocene–Eocene boundary (∼ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …

Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang, YK Chen-Wiegart, DV Kent - Proceedings of the National …, 2015 - osti.gov
The Paleocene–Eocene boundary (~ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …

[PDF][PDF] Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wanga, J Wangb, YK Chen-Wiegartb, DV Kentc - researchgate.net
Results In this study, we used a recently developed full-field hard X-ray ultrahigh-resolution
(∼ 30–50 nm without binning pixels) synchrotron-based transmission X-ray microscope …

Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wang, J Wang, YK Chen-Wiegart, DV Kent - 2015 - dspace.mit.edu
The Paleocene–Eocene boundary (∼ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …

[PDF][PDF] Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wanga, J Wangb, YK Chen-Wiegartb, DV Kentc - academia.edu
The Paleocene–Eocene boundary (∼ 55.8 million years ago) is marked by an abrupt
negative carbon isotope excursion (CIE) that coincides with an oxygen isotope decrease …

[PDF][PDF] Quantified abundance of magnetofossils at the Paleocene–Eocene boundary from synchrotron-based transmission X-ray microscopy

H Wanga, J Wangb, YK Chen-Wiegartb, DV Kentc - geology.rutgers.edu
Results In this study, we used a recently developed full-field hard X-ray ultrahigh-resolution
(∼ 30–50 nm without binning pixels) synchrotron-based transmission X-ray microscope …