Results 111 to 120 of about 946 (178)

Copper isotopes track the Neoproterozoic oxidation of cratonic mantle roots. [PDF]

Nat Commun
Chen C, Foley SF, Shcheka SS, Liu Y.
europepmc   +1 more source

Climate-change-enhanced habitat diversification for the Middle Jurassic Yanliao Biota in East Asia. [PDF]

Natl Sci Rev
Hao W, Yang J, Wang H, Mitchell RN, Zhang C, Qiu R, Guo J, Zhang W, Bao X, Deng C, Wang X, Hu Y, Yang JH, Zhu G, Zhou Z, Zhu R.   +15 more
europepmc   +1 more source

Mantle plume trail beneath the ca. 1.1 Ga North American Midcontinent Rift revealed by magnetotelluric data. [PDF]

Natl Sci Rev
Lin W, Schultz A, Yang B, Harris LB, Hu X.   +4 more
europepmc   +1 more source

Recent progress and future prospects of the early solar system chronology. [PDF]

Natl Sci Rev
Amelin Y, Yin QZ.
europepmc   +1 more source

Microbial life under Martian permafrost layer. [PDF]

Innovation (Camb)
Shang X, Huang R, Sun W.
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Asynchronous transfer of magmas and mineralizing fluids in a plutonic-subvolcanic-volcanic plumbing system. [PDF]

Sci Rep
Paoli G, Dini A, Vezzoni S, Ovtcharova M, Rocchi S.   +4 more
europepmc   +1 more source

Mantle oxidation by sulfur drives the formation of giant gold deposits in subduction zones. [PDF]

Proc Natl Acad Sci U S A
He DY, Qiu KF, Simon AC, Pokrovski GS, Yu HC, Connolly JAD, Li SS, Turner S, Wang QF, Yang MF, Deng J.   +10 more
europepmc   +1 more source

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Why metasomatic fronts are really metasomatic sides

Geology, 1995
Back-scattered electron microscope images of metasomatic calc-silicate rocks demonstrate complex mineral growth patterns; often oscillatory zoning defines a euhedral or subhedral morphology. We infer from this the existence of an appreciable transient porosity (up to a few percent) during metasomatic calc-silicate growth, and argue that porous ...
Bruce W. D. Yardley, Geoff E. Lloyd
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CLASSIFICATION OF METASOMATIC ROCKS AND FACIES OF SHALLOW METASOMATISM

International Geology Review, 1992
The authors present a dual but parallel classification of metasomatic rock types and metasomatic facies. The classification may make clearer to Westerners the meaning of some terms (eysite, secondary quartzite, etc.) used extensively only in the Russian literature.
N. Yu. Bardina, V. S. Popov
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Metasomatism and ophiolitic rocks

2022
Τα σερπεντινιωμένα υπερβασικά πετρώματα της Κεντρικής Εύβοιας εμφανίζονται στις περιοχές της Κύμης και του Παγώντα και χαρακτηρίζονται από διεισδύσεις φλεβών ροδιγκίτη. Οι εν λόγω ροδιγκίτες διακρίνονται στους ακόλουθους τέσσερις τύπους ανάλογα με τους πρωτόλιθους από τους οποίους προήλθαν: (i) ροδιγκίτες θολειϊτικών δολεριτών τύπου νησιώτικου τόξου ...
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