I agree that this site is using cookies. You can find further informations
here
.
X
Login
Merkliste (
0
)
Home
About us
Home About us
Our history
Profile
Press & public relations
Friends
The library in figures
Exhibitions
Projects
Training, internships, careers
Films
Services & Information
Home Services & Information
Lending and interlibrary loans
Returns and renewals
Training and library tours
My Account
Library cards
New to the library?
Download Information
Opening hours
Learning spaces
PC, WLAN, copy, scan and print
Catalogs and collections
Home Catalogs and Collections
Rare books and manuscripts
Digital collections
Subject Areas
Our sites
Home Our sites
Central Library
Law Library (Juridicum)
BB Business and Economics (BB11)
BB Physics and Electrical Engineering
TB Engineering and Social Sciences
TB Economics and Nautical Sciences
TB Music
TB Art & Design
TB Bremerhaven
Contact the library
Home Contact the library
Staff Directory
Open access & publishing
Home Open access & publishing
Reference management: Citavi & RefWorks
Publishing documents
Open Access in Bremen
zur Desktop-Version
Toggle navigation
Merkliste
1 Ergebnisse
1
Holocene thermal maximum mode versus the continuous warming..:
Chen, Fahu
;
Duan, Yanwu
;
Hao, Shuo
...
Science China Earth Sciences. 66 (2023) 8 - p. 1683-1701 , 2023
Link:
https://doi.org/10.1007/s11430-022-1113-x
RT Journal T1
Holocene thermal maximum mode versus the continuous warming mode: Problems of data-model comparisons and future research prospects
UL https://suche.suub.uni-bremen.de/peid=cr-10.1007_s11430-022-1113-x&Exemplar=1&LAN=DE A1 Chen, Fahu A1 Duan, Yanwu A1 Hao, Shuo A1 Chen, Jie A1 Feng, Xiaoping A1 Hou, Juzhi A1 Cao, Xianyong A1 Zhang, Xu A1 Zhou, Tianjun PB Springer Science and Business Media LLC YR 2023 SN 1674-7313 SN 1869-1897 JF Science China Earth Sciences VO 66 IS 8 SP 1683 OP 1701 LK http://dx.doi.org/https://doi.org/10.1007/s11430-022-1113-x DO https://doi.org/10.1007/s11430-022-1113-x SF ELIB - SuUB Bremen
Export
RefWorks (nur Desktop-Version!)
Flow
(Zuerst in
Flow
einloggen, dann importieren)