@misc{BobosGoncalvesLimaetal.2019,
  author    = {Bobos, Iuliu and Goncalves, Ana and Lima, Luis and Noronha, Fernando and Sudo, Masafumi},
  title     = {Micas Ar-40/Ar-39 dating of hydrothermal events related with the post-orogenic W (+/- Sn), (Cu, Mo) mineralization from Borralha, Northern Portugal},
  series = {Life with Ore Deposits on Earth - 15th SGA Biennial Meeting 2019,},
  journal   = {Life with Ore Deposits on Earth - 15th SGA Biennial Meeting 2019,},
  number    = {1},
  publisher = {SGA Soc Geology Applied mineral depositis},
  address   = {Geneva},
  pages     = {353 -- 356},
  year      = {2019},
  abstract  = {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.},
  language  = {en}
}
@misc{BenDorNeugebauerEnzeletal.2020,
  author    = {Ben Dor, Yoav and Neugebauer, Ina and Enzel, Yehouda and Schwab, Markus J. and Tjallingii, Rik and Erel, Yigal and Brauer, Achim},
  title     = {Reply to comment on: Ben Dor, Yoav et al. : Varves of the Dead Sea sedimentary record. - In: Quaternary science reviews : the international multidisciplinary research and review journal. - 215 (2019), S. 173 - 184. - (ISSN: 0277-3791). - https://doi.org/10.1016/j.quascirev.2019.04.011},
  series = {Quaternary science reviews : the international multidisciplinary research and review journal},
  volume    = {231},
  journal   = {Quaternary science reviews : the international multidisciplinary research and review journal},
  publisher = {Elsevier},
  address   = {Amsterdam [u.a.]},
  issn      = {0277-3791},
  doi       = {10.1016/j.quascirev.2019.106063},
  pages     = {5},
  year      = {2020},
  abstract  = {In the comment on "Varves of the Dead Sea sedimentary record." Quaternary Science Reviews 215 (Ben Dor et al., 2019): 173-184. by R. Bookman, two recently published papers are suggested to prove that the interpretation of the laminated sedimentary sequence of the Dead Sea, deposited mostly during MIS2 and Holocene pluvials, as annual deposits (i.e., varves) is wrong. In the following response, we delineate several lines of evidence which coalesce to demonstrate that based on the vast majority of evidence, including some of the evidence provided in the comment itself, the interpretation of these sediments as varves is the more likely scientific conclusion. We further discuss the evidence brought up in the comment and its irrelevance and lack of robustness for addressing the question under discussion.},
  language  = {en}
}
@misc{AyzelIzhitskiy2018,
  author    = {Ayzel, Georgy and Izhitskiy, Alexander},
  title     = {Coupling physically based and data-driven models for assessing freshwater inflow into the Small Aral Sea},
  series = {Innovative Water Resources Management in a Changing Environment - Understanding and Balancing Interactions between Humankind and Nature},
  volume    = {379},
  journal   = {Innovative Water Resources Management in a Changing Environment - Understanding and Balancing Interactions between Humankind and Nature},
  editor    = {Xu, Z Peng},
  publisher = {Copernicus},
  address   = {G{\"o}ttingen},
  issn      = {2199-899X},
  doi       = {10.5194/piahs-379-151-2018},
  pages     = {151 -- 158},
  year      = {2018},
  abstract  = {The Aral Sea desiccation and related changes in hydroclimatic conditions on a regional level is a hot topic for past decades. The key problem of scientific research projects devoted to an investigation of modern Aral Sea basin hydrological regime is its discontinuous nature - the only limited amount of papers takes into account the complex runoff formation system entirely. Addressing this challenge we have developed a continuous prediction system for assessing freshwater inflow into the Small Aral Sea based on coupling stack of hydrological and data-driven models. Results show a good prediction skill and approve the possibility to develop a valuable water assessment tool which utilizes the power of classical physically based and modern machine learning models both for territories with complex water management system and strong water-related data scarcity. The source code and data of the proposed system is available on a Github page (https://github.com/SMASHIproject/IWRM2018).},
  language  = {en}
}
@misc{AlsemgeestSchroederBoettgeretal.2016,
  author    = {Alsemgeest, Jitse and Schr{\"o}der, S. and Boettger, Ute and Pavlov, S. G. and Weber, I. and Greshake, A. and Kn{\"o}fler, H. -R. and Altenberger, Uwe and H{\"u}bers, H. -W.},
  title     = {COMBINED RAMAN-LIBS STUDIES ON IRON SULFIDES TO INVESTIGATE THE EFECTS OF THE LIBS PLASMA ON THE MINERAL COMPOSITION.},
  series = {Monthly notices of the Royal Astronomical Society},
  volume    = {51},
  journal   = {Monthly notices of the Royal Astronomical Society},
  publisher = {Wiley-Blackwell},
  address   = {Hoboken},
  issn      = {1086-9379},
  pages     = {A147 -- A147},
  year      = {2016},
  language  = {en}
}