δ18O of O2 in a Tibetan Ice Core Constrains Its Chronology to the Holocene

Abstract Dating of the Tibetan ice cores is often challenging with great uncertainties. The significant age difference between the Guliya ice core (∼760 ka [thousand years]) and other Tibetan ice cores (Holocene origin) necessitates new approaches to resolve the inconsistency. Here, we present the a...

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Номзүйн дэлгэрэнгүй

Үндсэн зохиолчид:	Huanting Hu, Qiuyu Li, Wangbin Zhang, Shuang‐ye Wu, Jing Song, Ke Liu, Xiang Zou, Hongxi Pang, Maojun Yan, Shugui Hou
Формат:	Artigo
Хэл сонгох:	Inglês
Хэвлэсэн:	Wiley 2022-11-01
Цуврал:	Geophysical Research Letters
Нөхцлүүд:	Tibetan ice core trapped air delta‐18O chronology oxygen isotopes Holocene
Онлайн хандалт:	https://doi.org/10.1029/2022GL098368
Шошгууд:	Шошго нэмэх Шошго байхгүй, Энэхүү баримтыг шошголох эхний хүн болох!