Late Ordovician to mid-Silurian Benambran subduction zones in the Lachlan Orogen, southeastern Australia
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چکیده
منابع مشابه
The magnitude and duration of Late Ordovician-Early Silurian glaciation.
Understanding ancient climate changes is hampered by the inability to disentangle trends in ocean temperature from trends in continental ice volume. We used carbonate "clumped" isotope paleothermometry to constrain ocean temperatures, and thereby estimate ice volumes, through the Late Ordovician-Early Silurian glaciation. We find tropical ocean temperatures of 32° to 37°C except for short-lived...
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ژورنال
عنوان ژورنال: Australian Journal of Earth Sciences
سال: 2014
ISSN: 0812-0099,1440-0952
DOI: 10.1080/08120099.2014.903858