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Tracking lithospheric delamination and surface processes across the Messinian salinity crisis. [PDF]
Mouthereau F +7 more
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Geological and physicochemical characterization of Kobe Sorsa graphite deposit, Ethiopia. [PDF]
Emmiru BT, Tsegaye SG, Sahoo PR.
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Evolution of the Neoproterozoic Kareim Basin, north Arabian - Nubian shield. [PDF]
Sehsah H +3 more
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Rayleigh wave attenuation and phase velocity maps of the greater Alpine region from ambient noise. [PDF]
Roisenberg HB +4 more
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Correlated crustal and mantle melting documents proto-Tibetan Plateau growth. [PDF]
Li W +6 more
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A non‐collisional, accretionary Sveconorwegian orogen
Terra Nova, 2012Terra Nova, 25, 30–37, 2013AbstractThe late Mesoproterozoic Sveconorwegian orogen in southwest Baltica is traditionally interpreted as the eastward continuation of the Grenville orogen in Canada, resulting from collision with Amazonia, forming a central part in the assembly of the Rodinia supercontinent.
Slagstad, Trond +4 more
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Hydrothermal ore deposits in collisional orogens
Science Bulletin, 2019Hydrothermal ore deposits at convergent plate boundaries represent extraordinary metal enrichment in the continental crust. They are generally associated with felsic magmatism in extensional settings at high thermal gradients. Although their formation is common during accretionary orogeny, more and more ore deposits have been discovered recently in the
Yongfei, Zheng +5 more
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Delamination in collisional orogens
Geology, 1990During continental collision, the weight of the downgoing slab may lead to extensional shearing in the descending plate, permitting separation of the downdip, dense oceanic lithosphere from the adjacent lighter continental lithospher. Separation may occur by means of a lithosphere-penetrating normal-sense shear zone, by means of pure shear necking of ...
Paul E. Sacks, Donald T. Secor, Jr.
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A non‐collisional, accretionary Sveconorwegian orogen – Comment
Terra Nova, 2013In a stimulating contribution, Slagstad et al. (2013) propose to interpret the 500-km-wide Sveconorwegian orogen in Scandinavia as a non-collisional, accretionary orogen. They challenge the more widely held view that it is the product of a late Mesoproterozoic to early Neoproterozoic continent–continent collision, formed during welding of ...
Möller, Charlotte +5 more
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