Doklady Earth Sciences
Doklady Earth Sciences is a journal of the Presidium of the Russian Academy of Sciences. It contains English translations of papers published in Doklady Akademii Nauk (Proceedings of the Russian Academy of Sciences), which was founded in 1933 and is published 36 times a year. Doklady Earth Sciences includes materials from the following areas: geology, mineralogy, petrology, oceanology, geography, soil science, paleontology, geochemistry, and geophysics.
The Editorial Board of Doklady Akademii Nauk (Proceedings of the Russian Academy of Sciences) accepts new articles in the Russian language, formatted in accordance with the Rules for Authors. The article must be presented for publication by acting Russian or foreign members of the Russian Academy of Sciences.
Doklady Earth Sciences is a peer reviewed journal. We use open/single blind/double blind peer review formats. Our team of reviewers includes over 160 reviewers, both internal and external (70%). The average period from submission to first decision in 2017 was 3 days, and that from first decision to acceptance was 30 days. The final decision on the acceptance of an article for publication is made by the Editorial Board.
Any invited reviewer who feels unqualified or unable to review the manuscript due to the conflict of interests should promptly notify the editors and decline the invitation. Reviewers should formulate their statements clearly in a sound and reasoned way so that authors can use reviewer’s arguments to improve the manuscript. Personal criticism of the authors must be avoided. Reviewers should indicate in a review (i) any relevant published work that has not been cited by the authors, (ii) anything that has been reported in previous publications and not given appropriate reference or citation, (ii) any substantial similarity or overlap with any other manuscript (published or unpublished) of which they have personal knowledge.
The Role of Geomagnetic Anomalies in the O+ Concentration Distribution Considering the Seasonal Position of the Sun according to the Data from the Meteor-M Complex
Velocities of Present-Day Horizontal Movements in the Central Sector of the Greater Caucasus according to GPS Observations and Their Relation to Tectonics and the Deep Structure of the Earth’s Crust
To view the rest of this content please follow the download PDF link above.