(5) See, for example, Robert Morris' Continuous Project-Altered Daily (1969) the materials of which underwent changes during the work's existence and were eventually swept up and disposed of by the artist; also: Robert Morris, 'AntiForm
', Artforum, April (1968) Robert Morris, "Ant Form," Artforum, April 1968, reprinted in Continuous Project Altered Daily: The Writings of Robert Morris, Cambridge, Mass., MIT Press, 1993, p.
The Chako antiform
: A folded segment of the Greater Himalayan sequence, Nar valley, Central Nepal Himalayal.
The mineralization has been modelled with east and west dipping limbs to the antiform
assumed to be 300m in down-dip length each down to a vertical depth of 250m.
clearly a peculiar postmodern work bespeaking play, antiform
Northwest Fingerpost Hill 1 is situated in a large-scale antiform
which forms a distinct hill with some of the best outcrops of small-scale second-order folding in the project area.
The tanzanite deposits occur in the crest of the large Lelatema fold or antiform
, which is bounded by major faults parallel to the schistosity.
7e) refolded by the upright [F.sub.3] Lightening Creek antiform
ABSTRACT: The computer Strain Analysis methods developed by University College of Cork researchers llave permitted a large number of analysis and the characterization of finite strain in two different regions with contrasting geodynamic scenanos: The Talas Ala Tau (Tien-Shan, Kyrgyzs Republic) and the Somiedo Nappe and Narcea Antiform
(Cantabrian to West Asturian-Leonese Zone boundaw, NW of Spain).
The Valle Formation is gently folded--as, for instance, in the huge antiform
(plis de fond) of the Puerto Nuevo section.
Hassan identifies postmodern qualities as "antiform
(disjunctive, open), chance, anarchy, exhaustion/silence, process, participation, dispersal, rhetoric, parataxis, metonymy, anti-narrative;" this list, McGee and Handa argue, "aptly characterizes the world in which WPAs must function everyday" (2).
7) constitutes a relief related to the development of a complex shaped recent antiform
that is located near the coast line, overprinted on previous folded Alpujarride rocks belonging to the Internal Zones of the Betic Cordillera.
In this paper the first non-permanent GPS network devoted to quantify the present-day deformation in the Zafarraya Fault and the Sierra Tejeda antiform