Studies of the margin have provided the framework for a number of conceptual models aimed at understanding transform margin development worldwide.
A seismic stratigraphic study of the Antarctic Peninsula margin of the Central Bransfield Basin was conducted using seismic and bathymetric data.
A comprehensive apatite fission-track (AFT) study of the passive margin of western peninsular India between 12° and 16°N is used to reconstruct the denudation chronology of the continental hinterland.
In two studies the flowable composite extended to the cervical margin [ 75, 81], whereas in the other studies contamination of the margin with resin material was avoided [ 80, 82], which seems a relevant difference when looking at marginal adaptation.
More recently, the NSF established a multidisciplinary program dedicated to studies of the continental margins.
Other studies of delineation of the margins of type 0-IIb lesions using ME-NBI have reported successful delineation rates of 61%% (Oyama et al).
Detailed geological/geomorphological studies of the southern margin of the ranges, focusing on a fault block of Oligocene Miocene sedimentary rocks, have constrained the landscape evolution.
Recent petrological, structural and geochronological studies of the eastern margin of the Bohemian Massif (Czech Republic) suggest a conceptual geodynamical model to explain exhumation of lower crustal (20 kbar, 800 °C) felsic rocks.
We find support for our interpretation in previous studies of the Ebro margin.
For example, one study found that the margins of error (MOE) for certain Census Tracts increased over 80%% from the 2000 decennial census (Alexander 2002).
