Published 1988
| Version v1
Book
Hydro-chemistry of paleontology of depression of Tajikistan in Late chalk period
Description
In this chapter authors made conclusion that on formation of clayey layers of upper chalk did influence following factors: shallow sea basin and its relatively small dimensions, climate aridity, relatively nearness nutrition areas, frequent change sea transgressions its recessions
Additional details
Additional titles
- Original title (Russian)
- Палеогидрохимия тадйикскоы депресии в позднем мелу
Publishing Information
- Publisher
- Donish
- Imprint Place
- Dushanbe (Tajikistan)
- Imprint Title
- The hydro-chemical paleontology and migration forms of elements in the hyper genes zone
- Imprint Pagination
- 144 p.
- Journal Page Range
- p. 82-103
INIS
- Country of Publication
- Tajikistan
- Country of Input or Organization
- Tajikistan
- INIS RN
- 39097777
- Subject category
- S58: GEOSCIENCES;
- Resource subtype / Literary indicator
- Numerical Data
- Descriptors DEI
- BORON; CLAYS; EXPERIMENTAL DATA; GEOLOGIC FORMATIONS; GYPSUM; MINERALS; NUMERICAL DATA; POTASSIUM; SEDIMENTS; WATER
- Descriptors DEC
- ALKALI METALS; DATA; ELEMENTS; HYDROGEN COMPOUNDS; INFORMATION; METALS; MINERALS; NUMERICAL DATA; OXYGEN COMPOUNDS; SEMIMETALS; SILICATE MINERALS; SULFATE MINERALS
Optional Information
- Notes
- Imprint:Paleogidrohimiya i formi migratsii elementov v zone gipergeneza