Results 131 to 140 of about 384 (188)

Mountain building process of the Taiwan orogeny. [PDF]

open access: yesSci Adv
Tan E   +4 more
europepmc   +1 more source

Tracking lithospheric delamination and surface processes across the Messinian salinity crisis. [PDF]

open access: yesNat Commun
Mouthereau F   +7 more
europepmc   +1 more source

Evolution of the Neoproterozoic Kareim Basin, north Arabian - Nubian shield. [PDF]

open access: yesSci Rep
Sehsah H   +3 more
europepmc   +1 more source

Correlated crustal and mantle melting documents proto-Tibetan Plateau growth. [PDF]

open access: yesNatl Sci Rev
Li W   +6 more
europepmc   +1 more source

A non‐collisional, accretionary Sveconorwegian orogen

Terra Nova, 2012
Terra 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
openaire   +2 more sources

Hydrothermal ore deposits in collisional orogens

Science Bulletin, 2019
Hydrothermal 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
openaire   +2 more sources

Delamination in collisional orogens

Geology, 1990
During 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.
openaire   +1 more source

A non‐collisional, accretionary Sveconorwegian orogen – Comment

Terra Nova, 2013
In 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
openaire   +1 more source

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