Class information for: |
Basic class information |
Hierarchy of classes |
The table includes all classes above and classes immediately below the current class. |
| Cluster id | Level | Cluster label | #P |
|---|---|---|---|
| 3 | 4 | GEOSCIENCES, MULTIDISCIPLINARY//GEOCHEMISTRY & GEOPHYSICS//METEOROLOGY & ATMOSPHERIC SCIENCES | 1953906 |
| 0 | 3 | GEOCHEMISTRY & GEOPHYSICS//GEOSCIENCES, MULTIDISCIPLINARY//GEOLOGY | 272432 |
| 605 | 2 | GEOCHEMISTRY & GEOPHYSICS//MANTLE CONVECTION//MID OCEAN RIDGES | 14429 |
| 27182 | 1 | IZVESTIYA AKADEMII NAUK SSSR FIZIKA ZEMLI//SH KELKAR ARTS COMMERCE SCI//IRREGULAR OPERATOR EQUATION | 255 |
Terms with highest relevance score |
| rank | Category | termType | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|---|
| 1 | IZVESTIYA AKADEMII NAUK SSSR FIZIKA ZEMLI | journal | 312104 | 23% | 4% | 59 |
| 2 | SH KELKAR ARTS COMMERCE SCI | address | 247190 | 1% | 100% | 2 |
| 3 | IRREGULAR OPERATOR EQUATION | authKW | 164792 | 1% | 67% | 2 |
| 4 | REGULAR MULTIRESOLUTION ANALYSIS | authKW | 164792 | 1% | 67% | 2 |
| 5 | FINITE DIMENSIONAL APPROXIMATION SCHEME | authKW | 123595 | 0% | 100% | 1 |
| 6 | FINITE DIMENSIONAL APPROXIMATION SCHEME GRADIENT TYPE ITERATIVE METHOD | authKW | 123595 | 0% | 100% | 1 |
| 7 | GRADIENT TYPE ITERATIVE METHOD | authKW | 123595 | 0% | 100% | 1 |
| 8 | WAVELET LIKE SOLITONS | authKW | 123595 | 0% | 100% | 1 |
| 9 | WEAK AND APPROXIMATE WEAK SOLUTIONS TO INITIAL BOUNDARY VALUE PROBLEMS | authKW | 123595 | 0% | 100% | 1 |
| 10 | WEAK AND APPROXIMATE WEAK SOLUTIONS TO INITIAL BOUNDARY VALUE PROBLEMS FOR PARABOLIC EQUATIONS | authKW | 123595 | 0% | 100% | 1 |
Web of Science journal categories |
| chi_square_rank | Category | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | Geochemistry & Geophysics | 3499 | 33% | 0% | 83 |
| 2 | Geosciences, Multidisciplinary | 3320 | 42% | 0% | 107 |
| 3 | Multidisciplinary Sciences | 873 | 10% | 0% | 26 |
| 4 | Oceanography | 282 | 8% | 0% | 20 |
| 5 | Geology | 226 | 4% | 0% | 11 |
| 6 | Telecommunications | 3 | 2% | 0% | 4 |
| 7 | Engineering, Petroleum | 2 | 0% | 0% | 1 |
| 8 | Engineering, Geological | 1 | 0% | 0% | 1 |
| 9 | Gerontology | 1 | 0% | 0% | 1 |
| 10 | Physics, Mathematical | 1 | 1% | 0% | 3 |
Address terms |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | SH KELKAR ARTS COMMERCE SCI | 247190 | 1% | 100% | 2 |
| 2 | SUBBOTIN GEOPHYS | 9690 | 1% | 4% | 2 |
| 3 | GEOTHERMAL PROBLEMS | 3553 | 1% | 1% | 2 |
| 4 | DAGESTAN | 2628 | 0% | 2% | 1 |
| 5 | MIDT JOINT PHYS EARTH | 1565 | 1% | 1% | 2 |
| 6 | SHIRSHOV OCEANOL | 1267 | 1% | 0% | 3 |
| 7 | SCI TECHNOL UNIQUE RUMENTAT | 1111 | 0% | 1% | 1 |
| 8 | ORE DEPOSIT GEOL PETROG MINERAL GEOCHEM | 914 | 0% | 1% | 1 |
| 9 | MIDT UNITED PHYS EARTH | 560 | 0% | 0% | 1 |
| 10 | GEOSPHERE DYNAM | 547 | 0% | 0% | 1 |
Journals |
| chi_square_rank | term | chi_square | shrOfCwithTerm | shrOfTermInClass | termInClass |
|---|---|---|---|---|---|
| 1 | IZVESTIYA AKADEMII NAUK SSSR FIZIKA ZEMLI | 312104 | 23% | 4% | 59 |
| 2 | GEOPHYSICAL JOURNAL | 30891 | 2% | 6% | 4 |
| 3 | FIZIKA ZEMLI | 19114 | 5% | 1% | 12 |
| 4 | DOKLADY AKADEMII NAUK SSSR | 16097 | 21% | 0% | 53 |
| 5 | TIKHOOKEANSKAYA GEOLOGIYA | 12929 | 1% | 3% | 3 |
| 6 | OKEANOLOGIYA | 10351 | 5% | 1% | 14 |
| 7 | GEOTECTONICS | 7170 | 3% | 1% | 7 |
| 8 | IZVESTIYA-PHYSICS OF THE SOLID EARTH | 6577 | 4% | 1% | 9 |
| 9 | TECTONOPHYSICS | 3811 | 7% | 0% | 18 |
| 10 | JOURNAL OF GEODYNAMICS | 2619 | 2% | 0% | 6 |
Author Key Words |
Core articles |
The table includes core articles in the class. The following variables is taken into account for the relevance score of an article in a cluster c: (1) Number of references referring to publications in the class. (2) Share of total number of active references referring to publications in the class. (3) Age of the article. New articles get higher score than old articles. (4) Citation rate, normalized to year. |
Classes with closest relation at Level 1 |