Tienhsiang: Schists of Mesozoic metamorphosed melange

Complex metamorphic rock assemblage, including marble, greenschist, balckschist, chert, quartzite, etc. It is interpreted as metamorphosed mlange.

 

Uzϰa軡KۦK^(1986)uxWaϷ-xWaϻѡvCgٳaլdҥXAx_A@164CG

¦ ¦]QRWd (pelitic schist)AOܽ詥aDnۡCoض¦⪺c_۪Ὤ]nNwVnOF񪾥Ŭu@ӯUaAn_@ʤQAeפCܤKCH~Abܽ詥tLaϤ]Ppת¦bLC

bGQU@aϤWNDn¦aHPM5NAbQU@aϤWhH PM4 NAʫܬOաAѶ¦hܫphզCbLaϪ¦]۪MjzhAC@hpױqXQXءC¦b\ha謰ܦhpۭ^ߩҬAMY説ۤ]b¦C¦e`Ǧܶ¦ǦAӥB㦳o |}nzCeɦܲӲɡADncq]Aۭ^B BdۡBuBJ۩M۾Auۦɦܴ (porphyroblast) sbAHJ@a̬oFC¦쩥IniOI󬴽誺B⩥M⩥CH]٦¦۾AO]oǤtqhbʤ GHUAҥH]HϹΥ۾oӦW١C

cܽitt@حnۡAXSbܽaCMb_P賡hAObFn]g`b¦CDnephhΥYAMLܽ詥hA¦BhۤܽۦǩOM̱`@ͤ@_ۡChƥѰʤsyθHhܽӦC

d̥ۤDnAӲɩΤɡAe`ΦǺA㦳}nzCզqdۡBGۡBۭ^BѥۡB¶BuۤΨLqCdۤpױqƤبƤQءAp׬GQܤTQءCOFOWtɶKqɪDn򩥡Ab\hatɶKqeY説μhbzC

]Aܽ⩥Bۭ^BۼhM⩥ḀDnOѦUج⩥PۼhܽӦCǦAOq`]ƦӧeǽŦCzcybۤD`oFAbۤäۡCbӾ|ձahMζ¦@͡Cbjܽ詥Ϥɱ`M¦ΦKhAΦbDn``t¦hC

ܽۦǩ ܽۦǩӷ~W٥jz,oۦbܽtF_M賡Φ۪@aAQU@aϤWH PM2 NAOuӾ|ܽaCDnܽۦǩa__Ĭ᤽M˥H_AVnOFsHA`@ʤQCbH_¦hΥY説ۦǩ;qsVnOF]nӳ¨ˤWaϪ]``aMpY骬ܽۦǩA̫nݪDsҧtۦǩpF@ʤQءCsPܽۦǩhMY]bWzDnۦǩaXSA@ܽɪۤCܥiۦǩhΥYbnثeaϤWүݧԲӪaլdC

bDnۦǩaAo|̨}nܽۦǩbM˩MὬ]Ĭ᤽qCbo@aϥۦǩ̤jpױNQAѳoaϦVnAۦǩaUAӥBƤCۦǩ`MUؤhAPaIۦǩhpץiHqƤبXʤؤCܽۦǩeΫphAcӲɨʲɡA@TؤPCCLǩβ`Ǧ⪺ۦǩO̵oFӥB̦h; t~GجO¦Mզ⪺ۦǩAoxq֡AObӷ~WOȸؿvƩMs@˹~ۡCۦǩ]tDBΨLªӧe{SαamϮסAiHѸ˹ۧγ~CIJvTۦǩh`e{jPA{HC

bYzaIܽۦǩiHo{wgLܧΪƥۡA]AM (CɪiA1951) AoۥiH٤׬άۦǩCOuּƪͪ񤴵MOsӥiHŲO̪cCblXSۦǩo{iHѪƥۡAgŲw~ Schwagerina]H^AParafUSulina]H^A M Neoschwagerina]H^ݡCt~bӾb˵o{ƥ۳QŲw Waagenophyllum CҦoǤƥ۳ܥۦǩɥNOG|άOsxjͥNߴCoǤƥ۬OiHMwjnDɥNߤ@uC@ӻAjnDQ{OĤTC

bOWFAնΥն۱``Mܽۦǩ@͡CնObۦǩAL{t謰ҨNӳyAҥH`ۦǩMնL穥ۥX{CնHYBphBΤWh駨ͦbDnۦǩaApױqƤبƤQؤAhשMpתܤƤ]۷jCbܽۦǩa\hnնqɡAOHMsBMˡBMʤsTaQ{OIgٻȪqɡC

 

Figure 1.

Field Stop Location

Figure 2.

Black schist with highly deformed white marble layers indicating the nature of a Mesozoic mlange.

Figure 3.

U˨bѲGD C

Figure 4.

KBܽ誺C

Figure 5.

KBܽ誺C

Figure 6.

KBܽ誺C

Figure 7.

KBܽ誺ӡC

Figure 8.

 

Figure 9.

KBܽ誺ӡC

Figure 10.

賓ΤѮp C