From mboxrd@z Thu Jan 1 00:00:00 1970 X-Msuck: nntp://news.gmane.io/gmane.comp.tex.context/53243 Path: news.gmane.org!not-for-mail From: Xan Newsgroups: gmane.comp.tex.context Subject: Re: framedtext in naturaltables Date: Fri, 02 Oct 2009 13:29:12 +0200 Message-ID: <4AC5E408.7050507@telefonica.net> References: <4AC3AFE8.3080101@telefonica.net> Reply-To: mailing list for ConTeXt users NNTP-Posting-Host: lo.gmane.org Mime-Version: 1.0 Content-Type: multipart/mixed; boundary="------------070102030200020106010903" X-Trace: ger.gmane.org 1254510202 31439 80.91.229.12 (2 Oct 2009 19:03:22 GMT) X-Complaints-To: usenet@ger.gmane.org NNTP-Posting-Date: Fri, 2 Oct 2009 19:03:22 +0000 (UTC) Cc: mailing list for ConTeXt users To: Wolfgang Schuster Original-X-From: ntg-context-bounces@ntg.nl Fri Oct 02 21:03:14 2009 Return-path: Envelope-to: gctc-ntg-context-518@m.gmane.org Original-Received: from balder.ntg.nl ([195.12.62.10]) by lo.gmane.org with esmtp (Exim 4.50) id 1MtnPO-000462-7X for gctc-ntg-context-518@m.gmane.org; Fri, 02 Oct 2009 21:03:14 +0200 Original-Received: from localhost (localhost [127.0.0.1]) by balder.ntg.nl (Postfix) with ESMTP id 7D39EC9A8A; Fri, 2 Oct 2009 21:03:10 +0200 (CEST) X-Virus-Scanned: Debian amavisd-new at balder.ntg.nl Original-Received: from balder.ntg.nl ([127.0.0.1]) by localhost (balder.ntg.nl [127.0.0.1]) (amavisd-new, port 10024) with LMTP id RX6O9a18HRwH; Fri, 2 Oct 2009 21:03:07 +0200 (CEST) Original-Received: from balder.ntg.nl (localhost [127.0.0.1]) by balder.ntg.nl (Postfix) with ESMTP id E7835C9A90; Fri, 2 Oct 2009 21:03:06 +0200 (CEST) Original-Received: from localhost (localhost [127.0.0.1]) by balder.ntg.nl (Postfix) with ESMTP id 519D7C9A90 for ; Fri, 2 Oct 2009 21:03:05 +0200 (CEST) X-Virus-Scanned: Debian amavisd-new at balder.ntg.nl Original-Received: from balder.ntg.nl ([127.0.0.1]) by localhost (balder.ntg.nl [127.0.0.1]) (amavisd-new, port 10024) with LMTP id UudONJjqVitX for ; Fri, 2 Oct 2009 21:02:59 +0200 (CEST) Original-Received: from IMPaqm2.telefonica.net (impaqm2.telefonica.net [213.4.138.2]) by balder.ntg.nl (Postfix) with ESMTP id 7A9FFC9A8A for ; Fri, 2 Oct 2009 21:02:59 +0200 (CEST) Original-Received: from IMPmailhost5.adm.correo ([10.20.102.126]) by IMPaqm2.telefonica.net with bizsmtp id nkjm1c00D2jdgqJ3MnVHL8; Fri, 02 Oct 2009 13:29:17 +0200 Original-Received: from [172.26.0.7] ([83.55.62.93]) by IMPmailhost5.adm.correo with BIZ IMP id nnVD1c00T20iQ1P1lnVGlb; Fri, 02 Oct 2009 13:29:17 +0200 X-TE-authinfo: authemail="dxpublica" |auth_email="dxpublica@telefonica.net" X-TE-AcuTerraCos: auth_cuTerraCos="cosuitnetc02" User-Agent: Thunderbird 2.0.0.23 (X11/20090817) In-Reply-To: X-BeenThere: ntg-context@ntg.nl X-Mailman-Version: 2.1.12 Precedence: list List-Id: mailing list for ConTeXt users List-Unsubscribe: , List-Archive: List-Post: List-Help: List-Subscribe: , Original-Sender: ntg-context-bounces@ntg.nl Errors-To: ntg-context-bounces@ntg.nl Xref: news.gmane.org gmane.comp.tex.context:53243 Archived-At: This is a multi-part message in MIME format. --------------070102030200020106010903 Content-Type: text/plain; charset=ISO-8859-1; format=flowed Content-Transfer-Encoding: 7bit En/na Wolfgang Schuster ha escrit: > > Am 30.09.2009 um 21:22 schrieb Xan: > >> Hi, >> >> If I put >> \startframedtext[frame=off,background=screen,width=broad]....\stopframedtext >> in naturaltable, then I get that framed text passes table and that it >> aligns at top. >> >> Can you say me please how to get a right behaviour? > > \startframedtext[location=top,frame=off,background=screen,width=\dimexpr\hsize-\itemgrouplistwidth\relax] > > > or better > > \defineframedtext > [tableframed] > [location=top, > frame=off, > background=color, % screen works only with mkii but color with mkii > and mkiv > backgroundcolor=gray > width=\dimexpr\hsize-\itemgrouplistwidth\relax] > > \bTD\starttableframed ... \stoptableframed\eTD > > Wolfgang > It does not work: duplicate reference [][fig:smiley-semblants] on page 3 (copia -de-T1-Estructura-Externa-Terra-Roques-i-Minerals) ) (/usr/share/texmf/tex/context/base/pdfr-def.tex) systems : begin file copia-de-T1-Estructura-Externa-Terra-Roques-i-Mine rals at line 122 ! Undefined control sequence. \@@kdframedtextwidth ...size -\itemgrouplistwidth \startlocalframed ...h {\framedparameter \c!width }\edef \localheight {\fram... \dododostartframedtext ...#1][\c!strut =\v!no ,#3] \bgroup \let \\=\endgraf \... { ...expr \hsize -\itemgrouplistwidth ] { \bf \em Estructura interna... \handleTBLcell ...{\bTBLCELL \TBLcharalign {#2}{#4 }\eTBLCELL \inTBLcell {#1}... ... l.257 \eTABLE } ? at least in MKII. I attached the whole file. Thanks a lot, Xan. --------------070102030200020106010903 Content-Type: text/plain; name="copia-de-T1-Estructura-Externa-Terra-Roques-i-Minerals.context" Content-Disposition: inline; filename*0="copia-de-T1-Estructura-Externa-Terra-Roques-i-Minerals.conte"; filename*1="xt" Content-Transfer-Encoding: quoted-printable % interface=3Den output=3Dpdftex % Regime \enableregime[utf] % Choose a font \setupbodyfont [cmr,10pt] % Be tolerant with paragraph building \setuptolerance [horizontal,verytolerant,stretch] % Choose a language, and associated hyphenation rules. %\language [ca] \mainlanguage[ca] % Page number \setuppagenumbering [location=3D{footer}] % Paper size \setuppapersize [a4] % Margins %\setuplayout [grid=3Dyes, footer=3D0.5\footerheight, header=3D0.5\heade= rheight] %\setuplayout[footer=3D2cm, header=3D2cm] %\showlayout %\showframe %\showsetups \setuplayout[topspace=3D1.5cm,margin=3D1.5cm,header=3D0.8cm,footer=3D1.5c= m,width=3Dfit,height=3Dfit,backspace=3D1.7cm] % Enable colors and activate hyperlinks \setupcolors [state=3Dstart] %\definecolor[lightBlue][r=3D0.5, g=3D0.5, b=3D1.0] %\setupinteraction [state=3Dstart, color=3DlightBlue] %\setupurl[style=3Dsmall, space=3Dyes] \setupurl[space=3Dyes] % Enumerate the URLs %\useURL[wiki][http://wiki.contextgarden.net][][\ConTeXt\ wiki] % Fonts %% Chapters... \setupheads[align=3Dflushleft] \setuphead[chapter][style=3D{\tfd\bf}] \setuphead[section][style=3D{\ssbfc}, header=3Dnomarking] \setuphead[subsection][style=3D{\ssbfb}] \setuphead[subsubsection][style=3D{\bfa}] %\setuphead[section][textstyle=3Dbold] % Bibliography options % BIBTEX %\usemodule[bib] %\usemodule[bibltx] %\setupbibtex[database=3Dfuncions,sort=3Dauthor] %\setuppublications [alternative=3Dams,numbering=3Dyes, sorttype=3Dbbl, c= riterium=3Dall]% %\setupheadtext[ca][pubs=3DRefer=C3=A8ncies] %\setuppublicationlist[authoretallimit=3D3] %\setuppublicationlist[authoretaltext=3D{\it\ et al.}] %\setuppublicationlist[authoretaldisplay=3D1] %Indentation \setupheads[indentnext=3Dyes]=20 \setupindenting[yes,small,first] % Vertical spaces between paragraphs \setupwhitespace[none] %Itemize \setupitemize[each][identnext=3Dyes,margin=3D2em] \setupitemize[each][headstyle=3Dbold] % Mathematical packets %\usemodule[newmat] % Modules \usemodule[tikz] \usetikzlibrary[mindmap,arrows,calc] %\usetikzlibrary[trees] % AMSTHM \defineenumeration [exercici] [text=3D{Exercici},headstyle=3Dbold,between=3D\blank,titledistance=3D0e= m,textdistance=3D1em, stopper=3D{.\space},location=3Dserried,left=3D{\bgroup\bf},right=3D{\egro= up},width=3Dfit,headstyle=3D\ss] % Table of contents %% dots between... and subsubsubsection are not listed \setupcombinedlist[content][level=3D4,alternative=3Dc]=20 %% section =3D bold. % width=3D 10mm --> less space between num-letter %% line break after section. \setuplist[section][style=3Dbold,width=3D10mm]=20 \setuplist[section][before=3D\blank] %% margin =3D 10 mm. Put the subsection just bottom section. \setuplist[subsection][margin=3D10mm,width=3D10mm] \setuplist[subsubsection][margin=3D20mm,width=3D10mm] % Set "=C3=8Dndex" like "=C3=8Dndex de continguts" \setupheadtext [ca] [content=3D=C3=8Dndex] % Heads and footers \setupfootertexts[{\tfx \pagenumber/\lastpage}] \setupfooter[text][before=3D\hrule] \setupheader[text][after=3D\hrule] \setupheadertexts[{\tfx 4t DIVER CN. Tema 1 - Estructura Externa de la Te= rra}][{\tfx IES Binissalem. {\bf FULL 1}. \currentdate.}] % hyphenating \hyphenation{do-cu-ment} \hyphenation{subs-ti-tueix} \hyphenation{pro-ble-ma} \hyphenation{Ma-the-ma-tics} \hyphenation{Ma-the-ma-ti-cal} \hyphenation{es-crip-tu-ra} \hyphenation{ge-ne-ra-lit-za-ci=C3=B3} \hyphenation{va-ria-bles} % em =3D bf italic \setupbodyfontenvironment[default][em=3Ditalic] % underline \setupunderbar[alternative=3Db] % Start the text \starttext %\startcolumns[n=3D2] \startalignment[middle] {\scb Roques i Minerals} \stopalignment \smallskip \placefigure [here,none] [fig:taula-roques-i-minerals] {Caracter=C3=ADstiques de roques i minerals} {\bTABLE[frame=3Doff,align=3D{middle}] %\setupTABLE[1,2][1][leftframe=3Doff,rightframe=3Doff] \setupTABLE[r][1,2,3][topframe=3Don] \setupTABLE[r][3][bottomframe=3Don] \setupTABLE[c][each][rightframe=3Don,leftframe=3Don] %\setupTABLE[c][2][leftframe=3Don] \bTR[align=3Dmiddle] \bTD[align=3Dmiddle,nc=3D2] {\sc Composici=C3=B3}: Les roques i els minerals estan formats per {\em \bf mat=C3=A8ria inorg=C3= =A0nica}, que =C3=A9s diferent de la mat=C3=A8ria que compon els =C3=A9ss= ers vius \eTD \eTR \bTR[align=3Dmiddle] \bTD {\sc Definici=C3=B3 de Minerals}: \hairline Els minerals s=C3=B3n materials terrestres que formen les roques. Un mine= ral es defineix com una subst=C3=A0ncia: \startitemize[1] \item {\bf \em S=C3=B2lida}. L'estat f=C3=ADsic que apareixen els materia= ls ha de ser s=C3=B2lid. Els gasos i l'aigua no s=C3=B3n minerals. \item {\bf \em Natural}. Els materials artificials no s=C3=B3n minerals. \item {\bf \em Inorg=C3=A0nica}. Els compostos que formen els minerals s=C3= =B3n aquells que formen la mat=C3=A8ria que no est=C3=A0 viva \item \startframedtext[location=3Dtop,frame=3Doff,background=3Dscreen,wid= th=3D\dimexpr\hsize-\itemgrouplistwidth]=20 {\bf \em Estructura interna fixa i ordenada}. Les part=C3=ADcules que for= men els minerals estan {\bf \em \red{ordenades}} i ocupen un {\bf \em \re= d{lloc fix}} a l'espai. Qualsevol mostra d'un mateix mineral sempre t=C3=A9= la mateixa estructura. \stopframedtext \item {\bf \em Composici=C3=B3 qu=C3=ADmica determinada}. Tots els materi= als tenen una {\bf \em \red{f=C3=B3rmula qu=C3=ADmica fixa}}. Un material= sempre t=C3=A9 la mateixa proporci=C3=B3 de cada element que el forma. \stopitemize \eTD \bTD[align=3Dmiddle] {\sc Definici=C3=B3 de Roques}: \hairline Una roca =C3=A9s un {\em \bf \red{agregats}} (uni=C3=B3) {\bf \em \red{de= minerals}}. Poden estar formades per un sol mineral o per diversos miner= als. \startitemize[1] \item {\bf \em Formats per un sol mineral}. S=C3=B3n pocs freq=C3=BCents.= Per exemple, la {\em calc=C3=A0ria} (format per la {\em calcita}) \item {\bf \em Formats per diversos minerals}. El cas m=C3=A9s freq=C3=BC= ent. Per exemple, el {\em granit}, que est=C3=A0 format per tres minerals= : {\em quars}, {\em ortosa} i {\em mica}. \stopitemize En general, {\em \bf no tenen un forma fixa}. Sin=C3=B3 que varia fins i = tot amb el mateix tipus de roca. \hairline {\sc Exemples de Roques} \hairline Entre les roques hi ha el m=C3=A0rmol, l'arcilla, el conglomerat, la roca= calc=C3=A0ria, el granit, la lava, el carb=C3=B3, el marbre, etc. \hairline {\sc Exemples de Minerals} \hairline Podem destacar com a minerals: el diamant, l'or i la plata, el talc, la c= alcita, la magnetita, l'halita, la pirita, la fluorita, el guix i el quar= s. \eTD \eTR \bTR \bTD {\sc Composici=C3=B3 dels Minerals} \hairline Els minerals estan formats per uns components b=C3=A0sics: els elements q= u=C3=ADmics. Es coneixen 90 elements qu=C3=ADmics distints en la naturale= sa, per=C3=B2 nom=C3=A9s uns quants representen el 98\% de l'escor=C3=A7a= terrestre. \placetable[here,none][fig:1]{Geoelements}{\starttable[|c|c|c|c|] Element \VL \% mineral \VL Element \VL \% mineral \FR \HL Oxigen \VL 46 \VL Calci \VL 4 \MR \HL Silici \VL 27 \VL Sodi \VL 2,8 \MR \HL Alumini \VL 8 \VL Potasi \VL 2,6 \MR \HL Ferro \VL 5 \VL Magnesi \VL 2,1 \LR \HL \stoptable} Aquests elements s'anomenen {\em \bf geoelements} i s=C3=B3n els que form= en la majoria dels minerals. \hairline {\sc Escala de duresa de Mohs} \hairline \placetable[here,none][fig:2]{Mohs}{\starttable[|c|c|c|c|] Mineral \VL Duresa \VL Mineral \VL Duresa \FR \HL Talc \VL 1 \VL Ortosa \VL 6 \MR \HL Guix \VL 2 \VL Quars \VL 7 \MR \HL Calcita \VL 3 \VL Topazi \VL 8 \MR \HL Fluorita \VL 4 \VL Corind=C3=B3 \VL 9 \MR \HL Apatita \VL 5 \VL Diamant \VL 10 \LR \HL \stoptable} \eTD \bTD {\sc Les Propietats dels Minerals} \hairline Per a saber si dos minerals s=C3=B3n iguals, podem determinar la seva f=C3= =B3rmula qu=C3=ADmica (el que =C3=A9s molt car) o b=C3=A9 veure si tenen = exactament les mateixes {\em \bf propietats f=C3=ADsiques}. Aquestes s=C3= =B3n: \startitemize[1] \item {\bf \em Duresa}. La resist=C3=A8ncia a ser ratllat. Els minerals e= s classifiquen segons l'{\em \bf escala de duresa de Mohs}. \item {\bf \em Tipus de fractura}. La forma en la que es trenca el minera= l (en fragments plans, hexagonals, etc.) \item {\bf \em Color}. Varia segons el mineral. Poden ser semitransparent= s. \item {\bf \em Tipus de la ratlla}. Si ratllam amb un mineral un tros de = porcelana, s'hi aprecia un color de la ratlla deixat per la pols fina del= mineral. A vegades, aquest color no coincideix amb el color del mineral. \item {\bf \em Altres}. Densitat (el molt que pesa), fluoresc=C3=A8ncia (= hi a minerals fluorescents), gust (l'halita t=C3=A9 gust salat), etc. \stopitemize \bigskip \=20 \eTD \eTR \eTABLE} \placefigure [here,none] [fig:taula-roques-i-minerals] {Caracter=C3=ADstiques de roques i minerals} {\bTABLE[frame=3Doff,align=3D{left},background=3Dscreen] %\setupTABLE[1,2][1][leftframe=3Doff,rightframe=3Doff] %\setupTABLE[r][1,2,3][topframe=3Don] %\setupTABLE[r][3][bottomframe=3Don] %\setupTABLE[c][each][rightframe=3Don,leftframe=3Don] %\setupTABLE[c][2][leftframe=3Don] \bTR \bTD[nc=3D2,align=3Dmiddle] {\scb Els cristalls} \eTD \eTR \bTR \bTD %\startsimplecolumns[n=3D2] \startitemize[1] \item Les part=C3=ADcules que formen els minerals estan ordenades a l'esp= ai ocupant llocs fixos. Aquesta organitzaci=C3=B3 interna de les part=C3=AD= cules es coneix amb el nom d'{\bf \em estructura interna} \item En un mineral, pot passar que l'estructura interna es manifesti ext= ernament amb formes geom=C3=A8triques (un cub, un prime, etc.). En aquest= cas , es parla d'un {\em \bf cristall}. Hi ha minerals cristalitzats \item Si l'estrucura interna no es manifesta exteriorment, aleshores diem= que el mineral =C3=A9s un {\em \bf cos cristal=C2=B7l=C3=AD}. \stopitemize %\stopsimplecolumns \eTD \bTD[width=3D.5cm] \quad \eTD \bTD[width=3D4cm] {\externalfigure[figs/Cubic.png][scale=3D1000]} \eTD \eTR \eTABLE} \placefigure [here] [fig:smiley-semblants] {Minerals} {\startcombination[2*2] {\externalfigure[figs/Halita.jpg][scale=3D800]} {Halita} {\externalfigure[figs/Quartz.jpg][scale=3D150]} {Quars} {\externalfigure[figs/diamond.jpg][scale=3D700]} {Diamand} {\ex= ternalfigure[figs/Guix.jpg][scale=3D230]} {Guix} \stopcombination} \startexercici Per qu=C3=A8 el mercuri, un metall l=C3=ADquid, no es cons= idera com un mineral? \stopexercici \startexercici Quins s=C3=B3n els quatre geoelements m=C3=A9s abundants? \stopexercici \startexercici Si tenguessis un mineral de duresa 7,5 en l'escala de Mohs= , quins minerals podia ratllar? \stopexercici \startexercici De quina mat=C3=A8ria estan formats els minerals i les roq= ues? \stopexercici \startexercici Qu=C3=A8 diferencia les roques dels minerals? \stopexercici \startexercici Quines s=C3=B3n les caracter=C3=ADstiques principals que d= efineixen a un mineral? \stopexercici \page[yes] \placefigure [here] [fig:smiley-semblants] {Minerals} {\startcombination[2*1] {\externalfigure[figs/MagnetitaEZ.jpg][scale=3D300]} {Magnetita} {\externalfigure[figs/Pyrite.jpg][scale=3D1000]} {Pirita} \stopcombination} \placefigure [here] [fig:smiley-semblants] {Roques} {\startcombination[1*1] {\externalfigure[figs/caliza.jpg][scale=3D80]} {Calc=C3=A0ria} \stopcombination} \placefigure [here] [fig:smiley-semblants] {Roques} {\startcombination[2*1] {\externalfigure[figs/Conglomerat.jpg][scale=3D400]} {Conglomerat} {\externalfigure[figs/marmol.jpg][scale=3D800]} {M=C3=A0rmol} \stopcombination} %\stopcolumns \stoptext % Finish de text %\jobname --------------070102030200020106010903 Content-Type: text/plain; charset="us-ascii" MIME-Version: 1.0 Content-Transfer-Encoding: 7bit Content-Disposition: inline ___________________________________________________________________________________ If your question is of interest to others as well, please add an entry to the Wiki! maillist : ntg-context@ntg.nl / http://www.ntg.nl/mailman/listinfo/ntg-context webpage : http://www.pragma-ade.nl / http://tex.aanhet.net archive : https://foundry.supelec.fr/projects/contextrev/ wiki : http://contextgarden.net ___________________________________________________________________________________ --------------070102030200020106010903--