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| 1 | The Koshrabad granite massif in Uzbekistan: petrogenesis, metallogeny, and geodynamic setting显示文摘 | D.L. Konopelko Yu S. Biske K. Kullerud R. Seltmann F.K. Divaev | 2011 | Russian Geology and Geophysics2011，，12： | 1 |
| 2 | Selective seeding formagnetic separation显示文摘 | Hwang J Y Kullerud G Takayasu M | | 0，，06： | 1 |
| 3 | Chlorine, titanium and barium-rich biotites: Factors controlling biotite composition and implications for garnet-biotite geothermometry显示文摘 | Kullerud K | 1995 | Contributions to Mineral-ogy and Petrology1995，120，： | 1 |
| 4 | High-pressure fluid-rock reactions involving Cl-bearing fluids in lower-crustal ductile shear zones of the Flakstadoy Basic Complex, Lofoten, Nor- way显示文摘 | Kullerud K Flaat K Davidsen B | 2001 | Journal of Petrology2001，42，： | 1 |
| 5 | Chlorine-rich amphiboles: Interplay between amphibole composition and an evolving fluid 显示文摘 | Kullerud K | 1996 | European Journal of Mineralogy1996，8，： | 1 |
| 6 | Cl-scapolite, Cl-amphibole, and plagioclase equilibria in ductile shear zones at Nusfjord, Lofo- ten, Norway: Implications for fluid compositional evolution during fluid-mineral interaction in the deep crust 显示文摘 | Kullerud K Erambert M | 1999 | Geochimica et Cosmoehimica Acta1999，63，： | 1 |
| 7 | On the calculation of isochrones 显示文摘 | Kullerud L | 1991 | Chem Geol1991，87，2： | 1 |
| 8 | Thermal stability of pentlandite显示文摘 | Kullerud G | 1963 | The Canadian Mineralogist1963，7，3： | 1 |
| 9 | The FeS-ZnS system, a geological thermometer, Norsk 显示文摘 | Kullerud G | 1953 | Geol Tidsskr1953，32，： | 1 |
| 10 | Geochemical and metalogenic provinces: a discussion initiated by results from geochemical mapping across northern Fennoscandia显示文摘 | B(/o)lviken B Kullerud G Loucks R R | 1990 | Journal of Geochemical Exploration1990，39，： | 1 |
| 11 | Economical Potential of An Ultramafic Rock at The Kval ya Island, North Norway显示文摘A low-grade metamorphic ultramafic rock at the Kval ya Island, North Norway, shows Ni content up to 5 600 ppm, and an average content of 2 500 ppm Ni. Olivine is absent from the rock, and Ni is principally bonded in pentlandite, violarite and millerite. The rock might be considered as a low-grade ore, with 0.2wt%– 0.56wt% Ni. Other metals that might be of economic interest to extract from the rock include Co (from pentlandite and violarite), and Cr and Fe (from magnetite). | Anna Pryadunenko Kre Kullerud | 2013 | 矿物学报2013，33，S1： | 0 |
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