Fig. 1.54.

Mon, 2020-08-31 23:32 -- hwadmin
Summary: 
Fault plane dip angle (α) is larger than the critical deformation angle of bedrock (δ). 1 = gob; 2 = fault plane; 3 = subsidence steps.
Type: 
Figure
Sub Component: 
Normal
Slug: 
F54
Highwire: Type: 
fragment
HighWire: Journal/Corpus Code: 
csirobk
Highwire: pisa_id: 
csirobk;9781486312559/1/BK07898_ch01/F54
Highwire: pisa_master: 
csirobk;9781486312559/1/BK07898_ch01/F54
HighWire: Atom Path: 
/csirobk/9781486312559/9781486312559/SEC3/F54.atom
Highwire: cpath: 
/content/9781486312559/9781486312559/SEC3/F54
Image - Large: 
Highwire: cpathalias: 
/content/csirobk/9781486312559/9781486312559/SEC3/F54
Image - Medium: 
Highwire: Variants: 
expansion
Image - Small: 
Highwire: State: 
Released
Contributors: 
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<atom:contributor xmlns:atom="http://www.w3.org/2005/Atom" xmlns:hwp="http://schema.highwire.org/Journal" xmlns:nlm="http://schema.highwire.org/NLM/Journal" hwp:inherited="yes" nlm:contrib-type="author"><atom:name>James Barbato</atom:name><nlm:name name-style="western" hwp:sortable="Barbato James"><nlm:surname>Barbato</nlm:surname><nlm:given-names>James</nlm:given-names></nlm:name></atom:contributor>
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