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MARCH 22 TO APRIL 7, WASHINGTON Cherry Blossom Festival, including the Smithsonian Kite Festival; free performances on the Tidal Basin Stage, featuring music, dance, song and martial arts; world figure skating championships; a parade.
Recording a marine foreland basin stage that developed in the São Francisco plate during the Neoproterozoic early Paleozoic West Gondwana assembly, the Ediacaran deposits unconformably overlie Archean Paleoproterozoic metamorphic assemblages of the Sete Lagoas basement high and fill a series of kilometer-long grabens in the southern São Francisco basin.
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Although the initial rift development of the three basins is very similar, basin architecture, sedimentary infill and distribution differ considerably during the syn-rift sag to the drift basin stages.
Three structural architectures can be identified in the basin, the early-stage faults, the mid-stage faults and the late-stage faults.
The late stage basin-fill history of the fluvial Dupi Tila Group (Plio-Pleistocene) is described.
Therefore, precise examination of the sentinel lymph node can accurately predict the lymph node status of the entire lymph basin at early stages of cancer progression.
Although the Ordos Basin underwent multi-stage tectonic movements in the Late Mesozoic Cenozoic eras, the deformation was confined to the western margin and no significant tectonic events occurred in the central part.
Each of the three lacustrine sequence architectures stands for a particular stage of basin fill and reflects variable rates of basin subsidence.
The Paleogene succession of the western Himalayan foreland basin developed in two stages, i.e. syn-collisional stage and post-collisional stage.
The paleocurrent flows were eastwards and westwards during the early and late stages of basin development and northwards and southwards during its middle stage, indicating typical forearc basin sedimentation with longitudinal supply and lateral filling.
From top to bottom, the Chang 10 to Chang 8 members represent the early development stages of the basin; the Chang 7 represents the expansion stage; the Chang 6 represents the filling stage of the large-scale delta; the Chang 4 and 5 represent the short small-scale lake expansion, and Chang 3 to 1 represent filling of the lake basin (He 2003; Yu et al. 2001; Lin et al. 2008).
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CEO of Professional Science Editing for Scientists @ prosciediting.com