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Stray bottles were thrust over the barriers towards officers to cheers and chants of "Shame on you, we're human too".
During subsequent north south shortening (D2), open to isoclinal south southeast-oriented F2 foldsouth southeast-orientedoproterozoic successions oF2the inlier were thrust over the Archaean nuclei ofolds Gawler Craton.
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a Marin Headlands, prehnite-pumpellyite facies OPS imbricates at the western side of Black Sand Beach, Bonita Cove (Fig. 6), where basalt and chert (itself internally imbricated) is thrust over siliciclastic rocks.
Likewise, the Tejam Group of rocks are thrusted over by the Almora Group of rocks and consists of Pipalkoti and Berinag formations.
David Rothery, a professor of planetary geosciences, at the Open University, UK, commented: "The Himalayan mountains are being thrust over the Indian plate; there are two or three big thrust faults, basically.
Shortly after, a large portion of sea floor was thrust over the older Klamath terranes; much of it is still visible atop Vulcan and Chetco peaks.
Near Roseburg this contact is exposed at the Wild Safari Fault where the Late Jurassic Dothan Formation has been thrust over the Roseburg Formation.
In Curry County, the lower Rogue passes through the Galice Formation, metamorphosed shale and other rocks formed when a small oceanic basin in the merging Klamath terranes was thrust over other Klamath rocks about 155 million years ago.
I was tired of him before, and I have always been tired of him, but there was a Pink Alex narrative that was thrust over the top of him: that Alex is unlucky-in-love, that he is goofy and forlorn, that he just needs The Right Girl to come into the villa and make a fairy tale happen for him.
The ranges of the Canadian and Northern Rockies were created when thick sheets of Paleozoic limestones were thrust eastward over Mesozoic rocks during the mountain-building episode called the Laramide Orogeny (65 to 35 million years ago).
This boundary cuts across rocks preserving an earlier record of arc continent collision during the course of which continental crust was subducted to mantle depths and Cambrian mafic ultramafic island arc rocks were thrust westwards over late Neoproterozoic Cambrian passive margin sequences.
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