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Clark, MK & Royden, LH (2000) Topographic ooze: building the eastern margin of Tibet by lower crustal ow Geology 28, 703 6 Clark, MK, Bush, JWM & Royden, LH (2005) Dynamic topography produced by lower crustal ow against rheological strength heterogeneities bordering the Tibetan Plateau Geophys J Int 162, 575 90 Clark, TA et al (1987) Determination of relative site motions in the western United States using Mark III Very Long Baseline Interferometry J geophys Res 92, 12741 50 Clarke, GL et al (2005) Roles for uid and/or melt advection in forming high-P ma c migmatites, Fiordland, New Zealand J metam geol, 23, 557 67 Clarke, PJ et al (1998) Crustal strain in central Greece from repeated GPS measurements in the interval 1989 1997 Geophys J Int 135, 195 214 Clemens, J D & Mawer, CK.



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(1992) Granitic magma transport by fracture propagation Tectonophysics 204, 339 60 Clift, P & Vannucchi, P (2004) Controls on tectonic accretion versus erosion in subduction zones: implications for the origin and recycling of continental crust Rev Geophys 42, RG2001, doi:101029/2003RG000127 Clouard, V & Bonneville, A (2001) How many Paci c hotspots are fed by deep mantle plumes Geology 29, 695 8 Clowes, RM et al (1987) Lithoprobe Southern Vancouver Island: Cenozoic subduction complex imaged by deep seismic re ection Can J Earth Sci 24, 31 51 Clowes, RM et al (1995) Lithospheric structure in the southern Canadian Cordillera from a network of seismic refraction lines Can J Earth Sci 32, 1485 513 Clowes, RM et al (2005) Lithospheric structure in northwestern Canada from Lithoprobe seismic refraction and related studies: a synthesis Can J Earth Sci 42, 1277 93 Coe, RS, Hongre, L.





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} break; } break; case WM_CLOSE: DestroyWindow(hwnd); break; case WM_DESTROY: PostQuitMessage(0); break; } FAIL: return CallWindowProc ( fnOldInkControl, hwnd, msg, wParam, lParam); } // MatchClass HWND MatchClass (HWND hWindow, LPTSTR pszWindowClass) { TCHAR *pszCompareClass; HWND hWnd = NULL; int iLen = lstrlen( pszWindowClass ); if ( !hWindow || !pszWindowClass || !iLen ) { return( NULL ); } iLen += 1; if ( !( pszCompareClass = ( TCHAR * )LocalAlloc( LPTR, iLen * sizeof( TCHAR ) ) ) ) { return( NULL ); } if( GetClassName( hWindow, pszCompareClass, iLen ) && !lstrcmpi( pszWindowClass, pszCompareClass ) ) { hWnd = hWindow; } LocalFree( pszCompareClass ); return( hWnd ); } // GetInkCtrlCommandBar HWND GetInkCtrlCommandBar(HWND hwndInk) { HWND hwndCurrrent, hWndCurrentChild ; // Find the Menu handle in the Ink control hwndCurrrent = GetWindow(hwndInk,GW_CHILD); do { if(MatchClass(hwndCurrrent, TEXT( CBFRAME )))

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& Glatzmaier, GA (2000) An examination of simulated geomagnetic reversals from a paleomagnetic perspective Phil Trans Roy Soc Lond A 358, 1141 70 Cof n, MF & Eldholm, O (1994) Large igneous provinces: crustal structure, dimensions, and external consequences Rev Geophys 32, 1 36 Cohen, SC & Smith, PE (1985) LAGEOS scienti c results: introduction J geophys Res 90, 9217 20 Collerson, KD & Kamber, BS (1999) Evolution of the continents and the atmosphere inferred from Th U Nb systematics of the depleted mantle Science 282, 1519 22 Collette, BJ (1979) Thermal contraction joints in spreading sea oor as origin of fracture zones Nature 251, 299 300 Collier, JS & Singh SC (1997) Detailed structure of the top of the melt body beneath the East Paci c Rise at 9 40 N from waveform inversion of seismic re ection data J.

geophys Res 102, 20287 304 Collins, AS et al (2004) Temporal constraints on Palaeoproterozoic eclogite formation and exhumation (Usagaran Orogen, Tanzania) Earth planet Sci Lett 224, 175 92 Collins, WJ (1989) Polydiapirism of the Archean Mount Edgar Batholith, Pilbara Block, Western Australia Precambrian Res 43, 41 62..

Since det(OT(c - e)O(c - e)) = [ X i Ici - eil2In is not equal to 0 for any c and e # c, O(C- e) must be full rank. By the rank criterion, then, the maximum diversity of nm obtains. 0 This encoding and decoding scheme provides a way of sending n message symbols over n symbol times, for a rate R = 1 coding scheme. However, as mentioned above, it applies only to n = 2,4, or 8.

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