发文地区与机构
近年国家 / 地区发文量统计
| 国家 / 地区 | 发文量 |
|---|---|
| GERMANY (FED REP GER) | 105 |
| CHINA MAINLAND | 84 |
| Italy | 50 |
| France | 48 |
| USA | 37 |
| Czech Republic | 31 |
| Poland | 31 |
| Switzerland | 30 |
| India | 29 |
| Spain | 29 |
近年机构发文量统计
| 机构 | 发文量 |
|---|---|
| CENTRE NATIONAL DE LA RECHERCHE SCIENTI... | 35 |
| HELMHOLTZ ASSOCIATION | 26 |
| CHINA UNIVERSITY OF GEOSCIENCES | 25 |
| CHINESE ACADEMY OF SCIENCES | 20 |
| CZECH ACADEMY OF SCIENCES | 20 |
| GOETHE UNIVERSITY FRANKFURT | 19 |
| CONSIGLIO NAZIONALE DELLE RICERCHE (CNR... | 17 |
| CHINESE ACADEMY OF GEOLOGICAL SCIENCES | 14 |
| ETH ZURICH | 14 |
| SENCKENBERG GESELLSCHAFT FUR NATURFORSC... | 14 |
文章引用情况
1
Carboniferous-Permian magmatism and Mo-Cu (W) mineralization in the contact zone between the Maopolska and Upper Silesia Blocks (south Poland): an echo of the Baltica-Gondwana collision2
Deformation within the Cycladic subduction-exhumation channel: new insights from the enigmatic Makrotantalo nappe (Andros, Aegean)3
Paleosalinity evolution of the Paleogene perennial Qaidam lake on the Tibetan Plateau: climatic vs. tectonic control4
Interpretation of source rock depositional environment and age from seep oil, east coast of New Zealand5
Post-Variscan thermal history of the Intra-Sudetic Basin (Sudetes, Bohemian Massif) based on apatite fission track analysis6
Three-dimensional geological modeling supports a revised Burdigalian chronostratigraphy in the North Alpine Foreland Basin7
Nature and provenance of the Beishan Complex, southernmost Central Asian Orogenic Belt8
Geochronology, geochemistry, and Sr-Nd-Pb-Hf isotopes of the Zhunsujihua granitoid intrusions associated with the molybdenum deposit, northern Inner Mongolia, China: implications for petrogenesis and tectonic setting9
The Proterozoic of NW Mexico revisited: U-Pb geochronology and Hf isotopes of Sonoran rocks and their tectonic implications10
Petrogenesis of early Late Cretaceous Asa-intrusive rocks in central Tibet, western China: post-collisional partial melting of thickened lower crust