angular unconformityの例文

• An angular unconformity therefore exists along the anticline's crest.
• The surface of this angular unconformity truncates dipping strata comprising the folded and faulted Unkar Group.
• The carbonate buildup is up to 4 km thick and form an angular unconformity to the overlying Permian sediments.
• The Tonto Group units were deposited on an ancient erosion surface ( angular unconformity ) on the Vishnu Basement Rocks.
• A quarry north east of the camp actively extracted Carboniferous limestone in the 20th century and shows a geological angular unconformity.
• The contact between the Tonto Group and Unkar Group is a prominent angular unconformity, which is part of the Great Unconformity.
• A sequence of Cambrian to Lower Ordovician sediments of the Eriboll and Durness Groups lie above the Torridonian with an angular unconformity.
• Vallis Vale exposes some of Britain s most classic rock outcrops, exhibiting several of the most easily demonstrated examples of angular unconformity available.
• The contact between the Tapeats Sandstone and the Cardenas Basalt and rest of the folded and faulted Unkar Group is a prominent angular unconformity.
• The contact between the Tapeats Sandstone and Hatakai Shale and the rest of the angular unconformity, which is part of the Great Unconformity.
• The contact between the Tapeats Sandstone and Bass Formation and the rest of the angular unconformity, which is part of the Great Unconformity.
• The overlying Tonto Group is separated from the Dox Sandstone and the rest of angular unconformity, which is part of the Great Unconformity.
• The gap in the sedimentary record, called an Angular unconformity, represents about 70 million years of non-deposition and / or erosion.
• The contact between the Cardenas Basalt and the overlying Nankoweap Formation is an erosion surface that is a disconformity or even a slight angular unconformity.
• The upper contact, which is part of the Great Unconformity, of the Sixtymile Formation is a disconformity that laterally becomes an angular unconformity.
• An angular unconformity truncates progressively older ( lower ) parts of the underlying Pahrump Group starting in the southern part of the area and moving north.
• Second, an angular unconformity, with a dip of less than 10? separates the base of the Nankoweap Formation from the underlying Unkar Group.
• The contact between the overlying Tapeats Sandstone and the folded and faulted Nankoweap Formation is a prominent angular unconformity that is part of the Great Unconformity.
• The surface of this angular unconformity is quite irregular as differential erosion of the resistant basalt sill formed monadnocks that have been buried by Tapeats Sandstone.
• This uplift of the basin, near the end of the Westphalian, halted deposition and created the angular unconformity at the top of the Karadon Fm.