Geochronology and geochemistry of the T ongcheng ultrapotassic hypabyssal intrusions at the south‐western margin of the O rdos B lock, C hina: Constraints on the geodynamic processes beneath the N orth C hina C raton

2018 ◽  
Vol 54 (2) ◽  
pp. 819-834 ◽  
Author(s):  
Huan Xu ◽  
Jin‐hai Luo ◽  
Zhan‐li Ren ◽  
Guan‐xu Chen ◽  
Yi‐fei Li ◽  
...  
2021 ◽  
Vol 356 ◽  
pp. 106104
Author(s):  
D.R. Mole ◽  
P.C. Thurston ◽  
J.H. Marsh ◽  
R.A. Stern ◽  
J.A. Ayer ◽  
...  

2018 ◽  
Author(s):  
Kai Cao ◽  
Guocan Wang ◽  
Philippe Hervé Leloup ◽  
Wei Mahéo ◽  
Yadong Xu ◽  
...  

2021 ◽  
pp. M55-2018-37 ◽  
Author(s):  
Karsten M. Haase ◽  
Christoph Beier

AbstractYoung volcanic centres of the Bransfield Strait and James Ross Island occur along back-arc extensional structures parallel to the South Shetland island arc. Back-arc extension was caused by slab rollback at the South Shetland Trench during the past 4 myr. The variability of lava compositions along the Bransfield Strait results from varying degrees of mantle depletion and input of a slab component. The mantle underneath the Bransfield Strait is heterogeneous on a scale of approximately tens of kilometres with portions in the mantle wedge not affected by slab fluids. Lavas from James Ross Island east of the Antarctic Peninsula differ in composition from those of the Bransfield Strait in that they are alkaline without evidence for a component from a subducted slab. Alkaline lavas from the volcanic centres east of the Antarctic Peninsula imply variably low degrees of partial melting in the presence of residual garnet, suggesting variable thinning of the lithosphere by extension. Magmas in the Bransfield Strait form by relatively high degrees of melting in the shallow mantle, whereas the magmas some 150 km further east form by low degrees of melting deeper in the mantle, reflecting the diversity of mantle geodynamic processes related to subduction along the South Shetland Trench.


1964 ◽  
Vol S7-VI (4) ◽  
pp. 545-553 ◽  
Author(s):  
Fernand Touraine

Abstract The Sainte-Victoire mountain in southern France has been considered the overturned southern limb of the Vauvenargues anticline, but the structure east of the Delubre fault is complicated by an oblique fold. The western margin is concealed by transgressive Tortonian (middle Miocene) beds covering the plateau of Beaumettes. The anticline probably is upper Cretaceous. Folding was renewed in the upper Lutetian (middle Eocene), and resulted in overturning and thrust faulting of the south limb. Subsequent normal faulting compartmented the mass, resulting in selective differential movement of blocks as horsts and grabens. The term piano keys structure is given to this type of structure.


2018 ◽  
Vol 98 ◽  
pp. 331-344 ◽  
Author(s):  
Stacey C. Priestley ◽  
Timothy E. Payne ◽  
Jennifer J. Harrison ◽  
Vincent E.A. Post ◽  
Paul Shand ◽  
...  

2009 ◽  
Vol 71 (3-4) ◽  
pp. 131-147 ◽  
Author(s):  
E. Malinverno ◽  
M.V. Triantaphyllou ◽  
S. Stavrakakis ◽  
P. Ziveri ◽  
V. Lykousis

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