نتایج جستجو برای: post collision volcanism

تعداد نتایج: 453614  

S.Z. Hosseini

Pleistocene basaltic lava flows, consisting of trachybasalt and basaltic trachyandesite, cover an area north-northwest of Shahre-Babak in southeastern Iran. The whole rock chemistry indicates that the lavas are dominantly alkaline and mildly calc-alkaline. Variation diagrams of SiO2 with major and trace elements are consistent with fractional crystallization processes involving olivine, pyroxen...

2016
Eric Font Thierry Adatte Alcides Nobrega Sial Luiz Drude de Lacerda Gerta Keller Jahnavi Punekar

The contribution of the Deccan Traps (west-central India) volcanism in the CretaceousPaleogene (KPg) crisis is still a matter of debate. Recent U-Pb dating of zircons interbedded within the Deccan lava flows indicate that the main eruptive phase (>1.1 × 106 km3 of basalts) initiated ~250 k.y. before and ended ~500 k.y. after the KPg boundary. However, the global geochemical effects of Deccan vo...

2003
J. Geldmacher B. B. Hanan

[1] We report Hf isotope compositions of 79 lavas that record the early ( 5–95 Ma) history of the Galápagos plume volcanism. These include lavas from the Caribbean Large Igneous Province (CLIP; 95–70 Ma), the accreted Galápagos paleo-hot spot track terranes (54–65 Ma) of Costa Rica (Quepos, Osa and Burica igneous complexes), and the Galápagos hot spot tracks (<20 Ma) located on the Pacific seaf...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2016
Richard V Morris David T Vaniman David F Blake Ralf Gellert Steve J Chipera Elizabeth B Rampe Douglas W Ming Shaunna M Morrison Robert T Downs Allan H Treiman Albert S Yen John P Grotzinger Cherie N Achilles Thomas F Bristow Joy A Crisp David J Des Marais Jack D Farmer Kim V Fendrich Jens Frydenvang Trevor G Graff John-Michael Morookian Edward M Stolper Susanne P Schwenzer

Tridymite, a low-pressure, high-temperature (>870 °C) SiO2 polymorph, was detected in a drill sample of laminated mudstone (Buckskin) at Marias Pass in Gale crater, Mars, by the Chemistry and Mineralogy X-ray diffraction instrument onboard the Mars Science Laboratory rover Curiosity The tridymitic mudstone has ∼40 wt.% crystalline and ∼60 wt.% X-ray amorphous material and a bulk composition wit...

2003
J. Geldmacher B. B. Hanan

[1] We report Hf isotope compositions of 79 lavas that record the early ( 5–95 Ma) history of the Galápagos plume volcanism. These include lavas from the Caribbean Large Igneous Province (CLIP; 95–70 Ma), the accreted Galápagos paleo-hot spot track terranes (54–65 Ma) of Costa Rica (Quepos, Osa and Burica igneous complexes), and the Galápagos hot spot tracks (<20 Ma) located on the Pacific seaf...

1998
A. T. BASILEVSKY J. W. HEAD

The details of stratigraphic units and structures making up six coronae and their regional surroundings on Venus were examined using full resolution Magellan images and stereoscopic coverage. Altimetry and stereoscopic coverage were essential in establishing the local stratigraphic relationships and the timing of corona-related topography. The degree of preservation of signatures of earlier cor...

2018
Laurent Jolivet Kensaku Tamaki Marc Fournier

The respective tectonic effects of back arc spreading and continental collision in Asia are considered either as two independent processes or as closely interrelated. Extrusion tectonics assumes that the opening of the South China Sea and the left-lateral motion along the Red River fault are geometrically linked in a pull-apart manner. This model is not accepted by several workers because the s...

Journal: :International Journal of Earth Sciences 2022

Abstract The SHRIMP U–Pb dating of zircons from felsic subvolcanic rocks in the Carboniferous formations Intra-Sudetic Basin SW Poland verifies previous views on timing Late Palaeozoic magmatic activity this area and constrains links between regional tectonics intra-basinal volcanism mid-European Variscides. Two main stages magmatism are identified: late orogenic stage, Early Permian post-oroge...

2006
A. B. Watts D. T. Sandwell W. H. F. Smith P. Wessel

[1] The seafloor is characterized by numerous seamounts and oceanic islands which are mainly volcanic in origin. Relatively few of these features (< 0.1%), however, have been dated, and so little is known about their tectonic setting. One parameter that is sensitive to whether a seamount formed on, near, or far from a mid-ocean ridge is the elastic thickness, Te, which is a proxy for the long-t...

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