Fitting an ellipse to an arbitrary shape: implications for strain analysis

被引:118
作者
Mulchrone, KF [1 ]
Choudhury, KR
机构
[1] Natl Univ Ireland Univ Coll Cork, Dept Appl Math, Cork, Ireland
[2] Natl Univ Ireland Univ Coll Cork, Dept Stat, Cork, Ireland
关键词
ellipse; fitting; strain analysis; moments; weighting;
D O I
10.1016/S0191-8141(03)00093-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An ellipse can be fit to an arbitrary shape using a linear least squares approach applied to boundary data. Alternatively, this problem can also be solved by calculating the second moments of the entire region, a technique popular in image analysis applications. If the irregular shape can be approximated by a polygon then Greens theorem allows efficient calculation of the second moments. If the shape is pixelated then the second moments can be calculated by a simple summation process. By considering the behaviour of these fitting methods with increasing deformation it is shown that as an arbitrary shape passively deforms, the best-fit ellipse also behaves as if it were deforming passively. This implies that all techniques of strain analysis that were previously restricted to populations of elliptical objects may now be applied to populations of arbitrary shapes, provided the best-fit ellipse is calculated by one of the methods described here. Furthermore it implies that selective sampling based on shape or methods of weighting based upon shape are invalid and tend to bias the raw data. (C) 2003 Elsevier Ltd. All rights reserved.
引用
收藏
页码:143 / 153
页数:11
相关论文
共 42 条
[1]   USE OF IMAGE-ANALYSIS IN THE MEASUREMENT OF FINITE STRAIN BY THE NORMALIZED FRY METHOD - GEOLOGICAL IMPLICATIONS FOR THE ZONE-HOUILLERE (BRIANCONNAIS ZONE, FRENCH ALPS) [J].
AILLERES, L ;
CHAMPENOIS, M ;
MACAUDIERE, J ;
BERTRAND, JM .
MINERALOGICAL MAGAZINE, 1995, 59 (395) :179-187
[2]   REFINEMENTS TO THE FRY METHOD (1979) USING IMAGE-PROCESSING [J].
AILLERES, L ;
CHAMPENOIS, M .
JOURNAL OF STRUCTURAL GEOLOGY, 1994, 16 (09) :1327-1330
[3]  
Anderson TW., 1984, INTRO MULTIVARIATE S
[4]  
[Anonymous], 1977, GEOLOGIE MINJB
[5]   Strain in ductile shear zones in the Caledonides of northern Sweden: a three-dimensional puzzle [J].
Bhattacharyya, P ;
Hudleston, P .
JOURNAL OF STRUCTURAL GEOLOGY, 2001, 23 (10) :1549-1565
[6]   ANALYSIS OF STRAINED SEDIMENTARY FABRICS - REVIEW AND TESTS [J].
BORRADAILE, GJ .
CANADIAN JOURNAL OF EARTH SCIENCES, 1987, 24 (03) :442-455
[7]   A new structural model for the SW Irish Variscides - The Variscan front of the NW European Rhenohercynian [J].
Bresser, G ;
Walter, R .
TECTONOPHYSICS, 1999, 309 (1-4) :197-209
[8]   A TECHNIQUE OF FINITE STRAIN ANALYSIS USING ELLIPTICAL PARTICLES [J].
DUNNET, D .
TECTONOPHYSICS, 1969, 7 (02) :117-&
[9]   NONRANDOM SEDIMENTARY FABRICS AND THEIR MODIFICATION BY STRAIN [J].
DUNNET, D ;
SIDDANS, AWB .
TECTONOPHYSICS, 1971, 12 (04) :307-&
[10]  
ELLIOTT D, 1970, GEOL SOC AM BULL, V81, P2221, DOI 10.1130/0016-7606(1970)81[2221:DOFSAI]2.0.CO