<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blakney, Barton Jeremy</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Architecture of tidally influenced point bars</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://search.proquest.com/docview/304960713</style></url></web-urls></urls><pub-location><style face="normal" font="default" size="100%">University of Alberta</style></pub-location><volume><style face="normal" font="default" size="100%">Earth and Atmospheric Sciences</style></volume><pages><style face="normal" font="default" size="100%">103</style></pages><language><style face="normal" font="default" size="100%">en</style></language><abstract><style face="normal" font="default" size="100%">Successions of inclined heterolithic stratification (IHS) within the McMurray Formation, northeastern Alberta, comprise stacked, genetic units averaging 6 to 10 m in thickness. Within the McMurray Type Section, these units are interpreted to represent the growth stages of a large, meandering channel deposited within the middle estuary.

Characterization of several modern, tidally-influenced depositional systems yielded the following generalizations: (1) a tripartite zonation of tidally-influenced systems is identifiable; (2) channel abandonments are rare within tide-dominated channel reaches; (3) large meander scroll bars form in systems with comparatively high fluvial input; and (4) tidally-influenced channels maintain lower sinuosity values than their fluvial counterparts.</style></abstract><issue><style face="normal" font="default" size="100%">M. Sc.</style></issue><custom1><style face="normal" font="default" size="100%">Geology</style></custom1><custom2><style face="normal" font="default" size="100%">Fort McMurray Formation</style></custom2><custom3><style face="normal" font="default" size="100%">http://www.worldcat.org/oclc/144362463</style></custom3><custom4><style face="normal" font="default" size="100%">Science</style></custom4></record></records></xml>