Late Holocene (2 ka) sea level, river discharge and climate interrelationship in the Taiwan region

Ping.-Mei Liew, Meng.-Long Hsieh

Open source

DOI: 10.1016/s1367-9120(99)00081-4
Published: 2000-08
Container: Journal of Asian Earth Sciences
Publisher: Elsevier BV
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1016/s1367-9120-99-00081-4,
  title = {Late Holocene (2 ka) sea level, river discharge and climate interrelationship in the Taiwan region},
  author = {Ping.-Mei Liew and Meng.-Long Hsieh},
  year = {2000},
  journal = {Journal of Asian Earth Sciences},
  doi = {10.1016/s1367-9120(99)00081-4},
  url = {https://doi.org/10.1016/s1367-9120(99)00081-4}
}

RIS

TY  - JOUR
TI  - Late Holocene (2 ka) sea level, river discharge and climate interrelationship in the Taiwan region
AU  - Ping.-Mei Liew
AU  - Meng.-Long Hsieh
PY  - 2000
JO  - Journal of Asian Earth Sciences
DO  - 10.1016/s1367-9120(99)00081-4
UR  - https://doi.org/10.1016/s1367-9120(99)00081-4
ER  -

APA

Liew, P., & Hsieh, M. (2000). Late Holocene (2 ka) sea level, river discharge and climate interrelationship in the Taiwan region. Journal of Asian Earth Sciences. https://doi.org/10.1016/s1367-9120(99)00081-4

Source records

crossref · retrieved 2026-09-27T00:43:46.492Z