Results 211 to 220 of about 30,947 (278)

Ancient plume-reinforced lithosphere modulates present-day crustal fluid migration and deformation. [PDF]

Nat Commun
Zhou Z, Yu N, Li X, Zhang S, Wang T, Kong W, Li T.   +6 more
europepmc   +1 more source

The global distribution of CO₂-rich magmas is determined by lithospheric thickness. [PDF]

Nat Geosci
Bowman EE, Gibson SA, Sui S, Lebedev S.
europepmc   +1 more source

Ultra-depleted mantle source of basalts from the South Pole-Aitken basin. [PDF]

Nature
Zhou Q, Yang W, Chu Z, Zhu H, Yang S, Zeng X, Xue DS, Jia LH, Zhang G, Zhang H, Lin Y, Zhang H, Tian HC, Peng P, Zhang DP, Gu L, Li C, Wu FY.   +17 more
europepmc   +1 more source

Linking electrical anomalies in the upper mantle to petrological and geochemical heterogeneities. [PDF]

Natl Sci Rev
Yang X, Xu YG, Xia QK.
europepmc   +1 more source

Devonian northward drift of the Qaidam-Kunlun continent constrains the early evolution of the Paleo-Tethys Ocean. [PDF]

Natl Sci Rev
Song P, Ding L, Wu C, Zuza AV, Zhang L, Yue Y, Xie J.   +6 more
europepmc   +1 more source

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Basalt

2021
Canadian Literature, No.
openaire   +2 more sources

The Columbia River Basalt

Science, 1982
Between 17 million and 6 million years ago, 200,000 square kilometers of the American Northwest were flooded by basaltic lava that erupted through fissures in the crust up to 150 kilometers long. Larger individual eruptions covered over a third of the Columbia Plateau in a few days. The lavas represent partial melts of the earth's mantle that were only
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Rare Earth Elements in Abyssal Basalts and Plateau Basalts

Nature Physical Science, 1971
IT is current practice to compare the abundances of the rare Earth elements (REE) in various rocks as well as in lunar materials with those in chondrites when exploring their origins. It should be emphasized that Masuda–Coryell plotting (Masuda1, 1962; Coryell et al.2, 1963) played an important part in studies of REE abundances in terrestrial and ...
NOBORU NAKAMURA, AKIMASA MASUDA
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The Basalt of Patagonia

Journal of science of the Hiroshima University. Series C, Geology and mineralogy, 1975
The samples subjected to the microscopic examination and chemical analysis were provided by the 4th Scientific Expedition to Patagonia by Hiroshima & Hokkaido Univ., 1969. The party collected them on the continental side of the southern Andes between Mendoza and Santa Cruz in Argentina.
TAKAMURA, Hajime, YOSHIDA, Hironao
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