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anticlinoria

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Journal Article
Journal: Geosphere
Published: 24 March 2021
Geosphere (2021) 17 (3): 932–956.
.... Rock uplift rates at the crests of two major anticlinoria are 0.9–4.9 mm/yr, and the dip-slip rate along the blind fault system that underlies these folds is 5.6–6.7 mm/yr. These rates are similar to those reported from the Ventura area to the southeast and indicate that the relatively high rates...
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Journal Article
Published: 01 October 2020
Russ. Geol. Geophys. (2020) 61 (10): 1156–1172.
FIGURES | View All (14)
Journal Article
Journal: GSA Bulletin
Published: 20 February 2020
GSA Bulletin (2020) 132 (9-10): 2105–2118.
FIGURES | View All (7)
Journal Article
Published: 01 November 2019
Russ. Geol. Geophys. (2019) 60 (11): 1310–1318.
... protrusion, between the Zyuratkul’ and Main Urals faults, there are no magnetic sources in the granite layer. As follows from the simulation results, in Taratash anticlinoria in the upper layer, the magnetic blocks are located directly above the rise of the basalt layer and the basite-ultrabasite belt...
FIGURES
Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0047(01)
EISBN: 9780813756479
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2012
GSA Bulletin (2012) 124 (3-4): 352–367.
... Mountain and Sutton–Notre Dame Mountains anticlinoria ( Fig. 1 ). S 3 can easily be traced across strike into Silurian and Devonian rocks of the Connecticut Valley Trough, where it is the earliest foliation. In the eastern part of the pre-Silurian units, open-tight asymmetric F 4 folds are observed...
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Journal Article
Published: 01 December 2011
Journal of Sedimentary Research (2011) 81 (12): 859–873.
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 2011
AAPG Bulletin (2011) 95 (11): 1821–1849.
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 2011
AAPG Bulletin (2011) 95 (11): 1851–1882.
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Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0016(05)
EISBN: 9780813756165
Journal Article
Journal: GSA Bulletin
Published: 01 September 2009
GSA Bulletin (2009) 121 (9-10): 1409–1420.
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 2009
AAPG Bulletin (2009) 93 (3): 357–377.
... to as anticlinoria. The flank of an anticlinorium is typically marked by a set of approximately equal-size secondary anticlines and synclines. These in turn may contain sets of third-order folds, and so it goes. However, folds in nature do not look like systematic wave trains. Instead, they can change abruptly...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2007
GSA Bulletin (2007) 119 (7-8): 978–992.
... Mountains anticlinoria but also in structural windows or fault slivers through oceanic rocks of the Dunnage zone ( Figs. 1 and 2 ). Very low-grade rocks, analogous to those of the external zone do, however, reappear to the southeast of the anticlinoria, in the hanging wall of major normal faults...
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Journal Article
Published: 05 January 2007
Canadian Journal of Earth Sciences (2006) 43 (11): 1639–1651.
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2006
GSA Bulletin (2006) 118 (7-8): 897–912.
... of the Weeksboro-Lunksoos and Munsungun anticlinoria of north-central Maine indicate that they resulted from such an event. The Bean Brook gabbro intrudes the Hurricane Mountain mélange and other related sedimentary strata of continental derivation. The gabbro and associated Dry Way volcanics have MORB...
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Journal Article
Published: 01 January 2005
Bulletin de la Société Géologique de France (2005) 176 (1): 93–105.
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2004
AAPG Bulletin (2004) 88 (9): 1255–1276.
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Journal Article
Published: 25 February 2003
Canadian Journal of Earth Sciences (2003) 40 (2): 269–284.
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Journal Article
Journal: GSA Bulletin
Published: 01 December 2002
GSA Bulletin (2002) 114 (12): 1480–1504.
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Journal Article
Journal: GSA Bulletin
Published: 01 August 1998
GSA Bulletin (1998) 110 (8): 1060–1074.