ࠄੇч೽εഌᜐጔࣧӦᄽϯϐ֖က

ഌࣧӦɡԋዕ߻ഌࣧӦϐᅌᡂޑၸำǶ

კ 5.3.1 ࠄੇч೽εഌᜐጔࣧӦϐࣧӦᜪࠠᆶځᄬ೷ӦቫቫׇϩѲǶѠ

᡼Ջ೽߻ഌࣧӦޑᄬ೷ӦቫቫׇǴҗΠԶ΢٩ׇࣁӅԖ߻஭຋ቫׇǵӕ

஭຋ቫׇǵࡕ஭຋ቫׇǵаϷԋዕයޑ߻ഌࣧӦቫׇǹѠࠄࣧӦޑᄬ೷

ӦቫቫׇҗΠԶ΢٩ׇࣁ߻஭຋ቫׇǵӕ஭຋ቫׇǵࡕ஭຋ቫׇаϷ҂

ԋዕයޑ߻ഌࣧӦቫׇǹዊԥпഐޑᄬ೷ӦቫቫׇҗΠԶ΢٩ׇࣁ߻஭

຋ቫׇǵӕ஭຋ቫׇаϷࡕ஭຋ቫׇǶ

ಃϤക ่ፕ

ૈᆶΟفࢪ؇ᑈᡏޑ຾ᙟᑈ(progradation)Ԗᜢǹ᎜ෳ࣬ IV ࣁΠ೽ഌڵډుੇۭࣧ

ޑ؇ᑈᕉნǴӧ᎜ෳ࣬ύૈ࣮ډޑЫރϸ৔ёૈࣁੇۭ৻ޑ؇ᑈယᡏǶ

Ѡ᡼Ջ೽߻ഌࣧӦǵѠࠄࣧӦаϷዊԥпഐ஭຋ࣧӦޑਔޜϩթёឍញࠄੇ

ч೽εഌᜐጔࣧӦᄽϯޑ֖ကǶӧђಃΟइਔࠄੇч೽εഌᜐጔวػΑ΋سӈܿ

чɡՋࠄوӛޑ஭຋ࣧӦǴх֖ዊԥпഐᆶѠࠄࣧӦǶԾύཥШଆਔࠄੇч೽ε ഌᜐጔ຾ΕΑࡕ஭຋ਔයǴዊԥпഐ୴ᑈࡕ஭຋ቫׇ(ύཥШɡ౜ж)ǶԾ΢ཥШ ଆǴֈֺ৞۱ᆶύ୯εഌᜐጔ௹ӛ࿘ና׎ԋѠ᡼೷ξ஥Ǵ೷ξ಻ख़ᆶ݈༧ኙԔቹ ៜΑఁύཥШࡕѠ᡼Ջ೽߻ഌࣧӦᆶѠࠄࣧӦޑวػǶѠ᡼Ջ೽߻ഌࣧӦௗڙε ໆޑѠ᡼೷ξ஥؇ᑈނ୴ᑈǴวػࣁԋዕ(mature)ޑ߻ഌࣧӦǹѠࠄࣧӦҭڙډ

݈༧ኙԔޑቹៜǴ೷ԋኙԔΠഐǴ໻ௗڙϿໆޑѠ᡼೷ξ஥؇ᑈނ୴ᑈǴวػΑ

҂ԋዕ(immature)ޑ߻ഌࣧӦ(׳ཥШԿϞ)Ƕዊԥпഐ҂ڙډ݈༧ኙԔޑቹៜǴԿ Ϟϝᆢ࡭஭຋ࣧӦޑচᇮǴڀԖ஭຋ቫׇᆶࡕ஭຋ቫׇǶѠ᡼Ջ೽߻ഌࣧӦǵѠ ࠄࣧӦаϷዊԥпഐӧύཥШϐࡕޑࣧӦਣࢎǴᇥܴΑࠄੇч೽εഌᜐጔࣧӦϐ วػࣁ೏୏εഌᜐጔڙډ݈༧ኙԔ؇फ़ϐቹៜǴ٠җࠄԶчև౜Α҂ڙኙԔޑ೏

୏εഌᜐጔɡ҂ԋዕ߻ഌࣧӦɡԋዕ߻ഌࣧӦϐᅌᡂޑၸำǶ

ୖԵၗ਑

஭܃൛Ǵ2010Ǵࠄੇܿч೽εഌᜐጔޑᄬ೷ࠠᄊǴ୯ҥѠ᡼εᏢੇࢩࣴز܌ᅺγ

೷ᄽϯޑ؇ᑈइᒵ—ODP1148 ઠుੇ؇ᑈނύޑ᛾ᏵǶӦౚࣽᏢ຾৖Ǵಃ 19 ڔಃ 4 යǴಃ 539-544 ।Ƕ

මਁϲǵ؋ҏమǵ৪҉ᝬǵᎅឦϒǴ1996ǴѠࠄࣧӦϐ᎜ෳӦቫࣴزǶѠ᡼ҡݨ Ӧ፦Ǵಃ 30 යǴಃ 281-308 ।Ƕ

ֆ୯䲝ǵЦԟࡌǵଘᅔैǵ߉ድǴ2007Ǵࠄੇч೽ੇ࣬ύғࣚวػޑ༾ᡏϯҡ᛾

ᏵǶੇࢩӦ፦ᆶಃѤ䵣Ӧ፦Ǵಃ 27 ڔಃ 1 යǴಃ 79-85 ।Ƕ

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Chang, J.H., Yu, H.S., Hsu, H.H., Liu, C.S., 2012. Forebulge Migration in the late Cenozoic Western Taiwan Foreland Basin. Tectonophysics 578, 117-125.

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Hsu, H.H., Liu, C.S., Yu, H.S., Chang, J.H., Chen, S.C., 2013. Sediment dispersal and accumulation in tectonic accommodation across the Gaoping Slope, offshore Southwestern Taiwan (article in press).

Chang, J.H., Yu, H.S., Lee, T.Y., Hsu, H.H., Liu, C.S., Tsai, Y.T., Characteristics of the flexure response to the Manila Trench and their implications in Taiwan-Luzon convergence belt, South China Sea (submitting).