Variation of gypsum morphology along deep core SG-1, western Qaidam Basin (northeastern Tibetan Plateau) and its implication to depositional environments
Datos Bibliográficos
| ID | 14980932 |
|---|---|
| Autores | Jiao Li (0000-0001-6391-8343), Minghui Li (0000-0001-7847-9240), Xiaomin Fang (0000-0003-2808-8836), Zhengrong Wang (0000-0002-1342-7762), Weilin Zhang (0000-0002-4634-1324), Yibo Yang (0000-0002-4625-3367) |
| Año | 2017 |
| Volumen | 430 |
| Páginas | 71-81 |
| Fecha de publicación | 2017-02-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Quaternary International (JOURNAL) |
| Identificadores de la revista | ISSN: 1040-6182 • E-ISSN: 1873-4553 |
| Editorial | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.quaint.2015.12.102 |
| OpenAlex | W2405874043 |
| Idioma | EN |
| Citas recibidas | 1 |
| Referencias citadas | 61 |
Geochemistry · Geomorphology · Gypsum · Morphology (biology · Plateau (mathematics · Sedimentary depositional environment · Structural basin · Geochemistry and Geologic Mapping · Geological and Geochemical Analysis · Hydrocarbon exploration and reservoir analysis · Geology · Paleontology
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Late Pliocene–Quaternary evolution of redox conditions in the western Qaidam paleolake (NE Tibetan Plateau) deduced from Mn geochemistry in the drilling core SG-1
Late Holocene History of Waldsea Lake, Saskatchewan, Canada
Evaporite minerals of the lower 538.5 m sediments in a long core from the Western Qaidam Basin, Tibet
Evaporite minerals and geochemistry of the upper 400m sediments in a core from the Western Qaidam Basin, Tibet
Quaternary paleolake nutrient evolution and climatic change in the western Qaidam Basin deduced from phosphorus geochemistry record of deep drilling core SG-1
| Obras citantes distintas | 1 |
|---|---|
| Citas por año | 0,11 |
| Intervalo de citas | 2017 - 2017 (1) |
| Velocidad de citación | historical |
| Altamente citado | No |
| Tipos de cita | Neutras: 1 |