|
|
Member Login
|
|
|
|
|
|
|
|
|
 International Geological Congress,oslo 2008
|
 Integrated perspectives on ophiolites of Pakistan
|
|
Accretion of ancient oceanic crust as in ophiolites
|
|
Accretion of the oceanic lithosphere in an ultra-slow spreading oceanic basin: inference from the Alpine-Apennine ophiolites
|
|
Os behaviour in groundwater and its effect on the Os residence time of the ocean
|
|
Re-Os dating of pyrite generations and late hydrocarbons associated with gold deposits - post-Sveconorwegian construction of Norway’s Eidsvoll Au deposit
|
|
Timing of granite emplacement utilizing molybdenite 187Re-187Os geochronology (Cruachan Granite, Etive Complex, Scotland), and further insights into Re-Os decoupling
|
|
Re-Os age of molybdenite from the Karkonosze massive (SW Poland)
|
|
India’s journey using Re-Os to date reactivation of ancient sutures
|
|
Inventorying geological heritage in vast territories: First proposal for paraná state, brazil
|
|
Contemporary state and perspectives of landscape management and tourism in Valday National Park
|
|
Geoconservation and its place within nature conservation
|
|
Different approaches for the study of the geodiversity
|
|
The realities of the conservation of heritage sites - damage, too much or too little protection?
|
|
The contribution of classical goniometry to China mineralogy and museum
|
|
Zeolites and Swedish dominance in mineralogy from 1756 to 1776
|
|
Urban Hiärne’s geological inquiries in 1694
|
|
Norwegian geologists as foreign members of the Russian academy of sciences
|
|
Into the mountains: Norwegian geology around 1800
|
|
Did Esmark’s (1824) glacial theory impel the discovery of the "greenhouse" effect (Tyndall, 1861), lithospheric isostasy (Jamieson, 1882) and continental drift (Wegener, 1912)?
|
|
Challenges in late Cenozoic chronostratigraphy and definition of the Quaternary
|
|
|
|
|
|
|
|
Home |
Contact Us |
Help
