伸展しんてん構造こうぞう

伸展しんてん構造こうぞう（英語えいご：Extensional tectonics）是ぜ指ゆび在ざい地殼ちかく或ある岩石がんせき圈けん受張力りょく而造成ぞうせい的てき構造こうぞう。通常つうじょう在ざい大陸たいりく裂きれ谷だに ^[1]. 中ちゅう洋よう脊，弧こ後ご盆地ぼんち，分離ぶんり板ばん塊かたまり邊べ緣えん和わ被ひ動どう邊べ緣えん等とう皆みな能のう形成けいせい伸展しんてん構造こうぞう^[2]。最さい常見つねみ的てき是ぜ在ざい鏟形斷層だんそう内的ないてき滾たぎ動どう背せ斜はす（英語えいご：rollover anticline）和かず背せ脊塌垮地ち塹^[3]。在ざい走はし滑すべり斷層だんそう也有やゆう伸展しんてん構造こうぞう，如伸展しんてん走はし滑すべり體系たいけい（英語えいご：releasing bends of strike-slip fault）。它是當とう走はし滑すべり斷層だんそう沿走向こう錯開時じ，中間ちゅうかん的てき間隙かんげき，會かい產さん生せい了りょう一いち個こ延伸えんしん或ある擴張かくちょう帶たい^[4]。在ざい聚合板ばん塊かたまり邊べ緣えん，通常つうじょう伸展しんてん構造こうぞう較少，但ただし當とう大陸たいりく碰撞時とき，地殼ちかく增ぞう厚あつし擡もたげ升ます，由ゆかり於重力じゅうりょく垮塌，向むこう側がわ延のべ申さる也形成けいせい伸展しんてん構造こうぞう^[5] ^[6]。

參考さんこう文獻ぶんけん[编辑]

^ Kearey, P.; Klepeis, K.A.; Vine, F.J. (2009). "Continental rifts and rifted margins". Global Tectonics. WileyBlackwell. p. 153. ISBN 978-1-4443-0322-3
^ Park, R. G. (1997). Foundations of Structural Geology (3rd ed.). Psychology Press. p. 64. ISBN 978-0-7487-5802-9
^ White, R. S.; Hardman, R. F. P.; Watts, A. B.; Whitmarsh, R. B.; Ebinger, C. J.; Jackson, J. A.; Foster, A. N.; Hayward, N. J. (15 April 1999). "Extensional basin geometry and the elastic lithosphere". Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences. 357 (1753): 741–765. doi:10.1098/rsta.1999.0351. JSTOR 55068
^ Armijo, R.; Meyer, B.; Navarro, S.; King, G.; Barka, A. (2002), "Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault?" (PDF), Terra Nova, Wiley-Blackwell, 14 (2): 80–86, Bibcode:2002TeNov..14...80A, CiteSeerX 10.1.1.546.4111, doi:10.1046/j.1365-3121.2002.00397.x
^ Dunlap, J. W.; Fossen, H. (1998). "Early Paleozoic orogenic collapse, tectonic stability, and late Paleozoic continental rifting revealed through thermochronology of K-feldspars, southern Norway" (PDF). Tectonics. 17 (4): 604–620. Bibcode:1998Tecto..17..604D. doi:10.1029/98TC01603
^ Hartz, E. H.; Andresen, A.; Hodges, K. V.; Martin, M. W. (July 2000). "U–Pb and 40Ar/39Ar constraints on the Fjord Region Detachment Zone: A long-lived extensional fault in the central East Greenland Caledonides" (PDF). Journal of the Geological Society. 157 (4): 795–809. doi:10.1144/jgs.157.4.795. Archived from the original (PDF) on 2012-03-02

[”Kearey”-1] Kearey, P.; Klepeis, K.A.; Vine, F.J. (2009). "Continental rifts and rifted margins". Global Tectonics. WileyBlackwell. p. 153. ISBN 978-1-4443-0322-3

[”Park”-2] Park, R. G. (1997). Foundations of Structural Geology (3rd ed.). Psychology Press. p. 64. ISBN 978-0-7487-5802-9

[”White”-3] White, R. S.; Hardman, R. F. P.; Watts, A. B.; Whitmarsh, R. B.; Ebinger, C. J.; Jackson, J. A.; Foster, A. N.; Hayward, N. J. (15 April 1999). "Extensional basin geometry and the elastic lithosphere". Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences. 357 (1753): 741–765. doi:10.1098/rsta.1999.0351. JSTOR 55068

[”Armijo”-4] Armijo, R.; Meyer, B.; Navarro, S.; King, G.; Barka, A. (2002), "Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault?" (PDF), Terra Nova, Wiley-Blackwell, 14 (2): 80–86, Bibcode:2002TeNov..14...80A, CiteSeerX 10.1.1.546.4111, doi:10.1046/j.1365-3121.2002.00397.x

[”Dunlap”-5] Dunlap, J. W.; Fossen, H. (1998). "Early Paleozoic orogenic collapse, tectonic stability, and late Paleozoic continental rifting revealed through thermochronology of K-feldspars, southern Norway" (PDF). Tectonics. 17 (4): 604–620. Bibcode:1998Tecto..17..604D. doi:10.1029/98TC01603

[”Hartz”-6] Hartz, E. H.; Andresen, A.; Hodges, K. V.; Martin, M. W. (July 2000). "U–Pb and 40Ar/39Ar constraints on the Fjord Region Detachment Zone: A long-lived extensional fault in the central East Greenland Caledonides" (PDF). Journal of the Geological Society. 157 (4): 795–809. doi:10.1144/jgs.157.4.795. Archived from the original (PDF) on 2012-03-02

[1]

[2]

[3]

[4]

[5]

[6]