В.В. Мухина's scientific contributions
What is this page?
This page lists the scientific contributions of an author, who either does not have a ResearchGate profile, or has not yet added these contributions to their profile.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
It was automatically created by ResearchGate to create a record of this author's body of work. We create such pages to advance our goal of creating and maintaining the most comprehensive scientific repository possible. In doing so, we process publicly available (personal) data relating to the author as a member of the scientific community.
If you're a ResearchGate member, you can follow this page to keep up with this author's work.
If you are this author, and you don't want us to display this page anymore, please let us know.
Publications (4)
В настоящей работе представлены наиболее существенные результаты по биостратиграфии четвертичных отложений и палеоокеанологическим реконструкциям, полученные авторами в течение 2006-2008 гг. Все микропалеонтологические исследования, включая отбор проб для изотопно кислородного и изотопно-углеродного анализов, выполнены авторами данной работы. Биос...
The area is characterized by regional stratigraphic hiatus from the Early Miocene up to the Quaternary. Numerous
manganese nodules mostly of the Oligocene age are located on a bottom surface on Tertiary or Quaternary
deposits. Detailed micropaleontological research of a block of ancient dense clay covered by the manganese
crust is carried out. Radi...
The Tertiary sediments were found in two areas on the bottom surface or under a thin layer of the Quaternary sediments. Combined investigations into radiolaria, diatoms and planktonic foraminifera have shown a continuous sequence of biostratigraphic zones from the Late Eocene to the Early Miocene and the regional hiatus between 17 and 1 m.y. The Ea...
The modem understanding of the Quaternary oceanic sediments stratigraphy is discussed in terms of climatostratigraphic methods (the rations between the relatively cold-water and warm-water species, micropaleontologic paleotemperature analysis based on the structure of the planktonic foraminifera thanatocoenoses, oxygen isotope method) and biostrati...
