TY  - GEN
A1  - Braun, David R.
A1  - Aldeias, Vera
A1  - Archer, Will
A1  - Arrowsmith, J. Ramon
A1  - Baraki, Niguss
A1  - Campisano, Christopher J.
A1  - Deino, Alan L.
A1  - DiMaggio, Erin N.
A1  - Dupont-Nivet, Guillaume
A1  - Engda, Blade
A1  - Feary, David A.
A1  - Garello, Dominique I.
A1  - Kerfelew, Zenash
A1  - McPherron, Shannon P.
A1  - Patterson, David B.
A1  - Reeves, Jonathan S.
A1  - Thompson, Jessica C.
A1  - Reed, Kaye E.
T1  - Reply to Sahle and Gossa: Technology and geochronology at the earliest known Oldowan site at Ledi-Geraru, Ethiopia
T2  - Proceedings of the National Academy of Sciences of the United States of America
Y1  - 2019
U6  - https://doi.org/10.1073/pnas.1911952116
SN  - 0027-8424
N1  - Letter
VL  - 116
IS  - 41
SP  - 20261
EP  - 20262
PB  - National Acad. of Sciences
CY  - Washington
ER  - 
TY  - GEN
A1  - Geissman, John
A1  - Jolivet, Laurent
A1  - Rusmore, Margi
A1  - Niemi, Nathan
A1  - Schildgen, Taylor F.
T1  - Thank you to our 2018 peer reviewers
T2  - Tectonics
N2  - An essential, respected, and critical aspect of the modern practice of science and scientific publishing is peer review. The process of peer review facilitates best practices in scientific conduct and communication, ensuring that manuscripts published are as accurate, valuable, and clearly communicated. The over 216 papers published in Tectonics in 2018 benefit from the time, effort, and expertise of our reviewers who have provided thoughtfully considered advice on each manuscript. This role is critical to advancing our understanding of the evolution of the continents and their margins, as these reviews lead to even clearer and higher-quality papers. In 2018, the over 443 papers submitted to Tectonics were the beneficiaries of more than 1,010 reviews provided by 668 members of the tectonics community and related disciplines. To everyone who has volunteered their time and intellect to peer reviewing, thank you for helping Tectonics and all other AGU Publications provide the best science possible.
Y1  - 2019
U6  - https://doi.org/10.1029/2019TC005595
SN  - 0278-7407
SN  - 1944-9194
VL  - 38
IS  - 4
SP  - 1159
EP  - 1163
PB  - Hoboken
CY  - Wiley
ER  - 
TY  - GEN
A1  - Hugenschmidt, Johannes
A1  - Giannopoulos, Antonios
A1  - Tronicke, Jens
T1  - Foreword
T2  - Near surface geophysics
Y1  - 2019
U6  - https://doi.org/10.1002/nsg.12050
SN  - 1569-4445
SN  - 1873-0604
VL  - 17
IS  - 3
SP  - 199
EP  - 200
PB  - Wiley
CY  - Oxford
ER  - 
TY  - GEN
A1  - Rounsevell, Mark D. A.
A1  - Metzger, Marc J.
A1  - Walz, Ariane
T1  - Operationalising ecosystem services in Europe
T2  - Regional environmental change
Y1  - 2019
U6  - https://doi.org/10.1007/s10113-019-01560-1
SN  - 1436-3798
SN  - 1436-378X
VL  - 19
IS  - 8
SP  - 2143
EP  - 2149
PB  - Springer
CY  - Heidelberg
ER  - 
TY  - GEN
A1  - Nitze, Ingmar
A1  - Grosse, Guido
A1  - Jones, B. M.
A1  - Romanovsky, Vladimir E.
A1  - Boike, Julia
T1  - Author Correction: Nitze, I; Grosse, G; Jones, B.M.; Romanovsky, V.E.; Boike, J.: Remote sensing quantifies widespread abundance of permafrost region disturbances across the Arctic and Subarctic. - Nature Communications. - 9 (2018), 5423
T2  - Nature Communications
Y1  - 2019
U6  - https://doi.org/10.1038/s41467-019-08375-y
SN  - 2041-1723
VL  - 10
PB  - Nature Publ. Group
CY  - London
ER  - 
TY  - GEN
A1  - Stoltnow, Malte
A1  - Seifert, Thomas
A1  - Jeske, Tilman J.
A1  - Gilbricht, Sabine
A1  - Krause, Joachim
T1  - Contributions to the mineralogical and geochemical characterization of Fe-Sn-Zn-Cu-In skarn-type mineralization in the Schwarzenberg mining district, Germany
T2  - Life with Ore Deposits on Earth – 15th SGA Biennial Meeting 2019
N2  - The Schwarzenberg mining district in the western Erzgebirge hosts numerous skarn-hosted tin-polymetallic deposits, such as Breitenbrunn. The St. Christoph mine is located in the Breitenbrunn deposit and is the locus typicus of christophite, an iron-rich sphalerite variety, which can be associated with indium enrichment. This study presents a revision of the paragenetic scheme, a contribution to the indium behavior and potential, and discussion on the origin of the sulfur. This was achieved through reflected light microscopy, SEM-based MLA, EPMA, and bulk mineral sulfur isotope analysis on 37 sulfide-rich skarn samples from a mineral collection. The paragenetic scheme includes: a pre-mineralization stage of anhydrous calc-silicates and hydrous minerals; an oxide stage, dominated by magnetite; a sulfide stage of predominantly sphalerite, minor pyrite, chalcopyrite, arsenopyrite, and galena. Some sphalerite samples present elevated indium contents of up to 0.44 wt%. Elevated iron contents (4-10 wt%) in sphalerite can be tentatively linked to increased indium incorporation, but further analyses are required. Analyzed sulfides exhibit homogeneous delta S-34 values (-1 to +2 parts per thousand VCDT), assumed to be post-magmatic. They correlate with other Fe-Sn-Zn-Cu-In skarn deposits in the western Erzgebirge, and Permian vein-hosted associations throughout the Erzgebirge region.
Y1  - 2019
SP  - 1089
EP  - 1092
PB  - SGA Soc Geology Applied mineral  depositis
CY  - Geneva
ER  - 
TY  - GEN
A1  - Bobos, Iuliu
A1  - Goncalves, Ana
A1  - Lima, Luis
A1  - Noronha, Fernando
A1  - Sudo, Masafumi
T1  - Micas Ar-40/Ar-39 dating of hydrothermal events related with the post-orogenic W (+/- Sn), (Cu, Mo) mineralization from Borralha, Northern Portugal
T2  - Life with Ore Deposits on Earth – 15th SGA Biennial Meeting 2019,
N2  - Secondary mica minerals collected from the Santa Helena (W- (Cu) mineralization) and Venise (W-Mo mineralization) endogenic breccia structures were Ar-40/Ar-39 dated. The muscovite Ar-40/Ar-39 data yielded 286.8 +/- 1.2 (+/- 1 sigma) Ma (samples 6Ha and 11Ha) which reflect the age of secondary muscovite formation probably from magmatic biotite or feldspar alteration. Sericite Ar-40/Ar-39 data yielded 280.9 +/- 1.2 (+/- 1 sigma) Ma to 279.0 +/- 1.1 (+/- 1 sigma) Ma (samples 6Hb and 11Hb) reflecting the age of greisen alteration (T similar to 300 degrees C) where the W- disseminated mineralization occurs. The muscovite 40Ar/39Ar data of 277.3 +/- 1.3 (+/- 1 sigma) Ma and 281.3 +/- 1.2 (+/- 1 sigma) Ma (samples 5 and 6) also reflect the age of muscovite (selvage) crystallized adjacent to molybdenite veins within the Venise breccia. Geochronological data obtained confirmed that the W mineralization at Santa Helena breccia is older than Mo-mineralization at Venise breccia. Also, the timing of hydrothermal circulation and the cooling history for the W-stage deposition was no longer than 7 Ma and 4 Ma for Mo-deposition.
Y1  - 2019
UR  - https://www.researchgate.net/publication/337901420_Micas_40_Ar_39_Ar_dating_of_hydrothermal_events_related_with_the_post-orogenic_W_Sn_Cu_Mo_mineralization_from_Borralha_Northern_Portugal
IS  - 1
SP  - 353
EP  - 356
PB  - SGA Soc Geology Applied mineral  depositis
CY  - Geneva
ER  - 
TY  - GEN
A1  - Gudipudi, Venkata Ramana
A1  - Rybski, Diego
A1  - Lüdeke, Matthias K. B.
A1  - Kropp, Jürgen
T1  - Urban emission scaling - Research insights and a way forward
T2  - Environment and Planning B: Urban Analytics and City Science
Y1  - 2019
U6  - https://doi.org/10.1177/2399808319825867
SN  - 2399-8083
SN  - 2399-8091
VL  - 46
IS  - 9
SP  - 1678
EP  - 1683
PB  - Sage Publ.
CY  - London
ER  - 
TY  - GEN
A1  - Nakaten, Natalie Christine
A1  - Kempka, Thomas
T1  - Retraction: Techno-Economic Comparison of Onshore and Offshore Underground Coal Gasification End-Product Competitiveness. (Retraction of Vol 10, art no 1643, 2017)
T2  - Energies : open-access journal of related scientific research, technology development and studies in policy and management
Y1  - 2019
U6  - https://doi.org/10.3390/en12173253
SN  - 1996-1073
VL  - 12
IS  - 17
PB  - MDPI
CY  - Basel
ER  -