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板块会聚期地中海海脊增生复合体处沉积物去向——泥喷与俯冲和增生的量平衡 被引量:1

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摘要 泥火山常见于碰撞构造地带。地中海海脊增生复合体沿线泥丘的形成与Cretan地壳刚性体向海一侧的后冲断层有关。资料表明泥丘尺度差别挺大。ODP160航次对Milano和Napoli两个泥丘的钻探,得以了解其结构、年代、形成及迷一样的结构变化。本文首次对...
作者 Kopf.,A 张萍
出处 《海洋地质动态》 1999年第6期19-21,共3页 Marine Geology Letters
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  • 1马建华.地中海海岭的泥火山活动──大洋钻探计划第160航次最初成果[J].海洋地质动态,1996,12(9):11-13. 被引量:1
  • 2Kopf A,Deyhle A, Zuleger E. Evidence for deep fluid circulation and gas hydrate dissociation using boron and boron isotopes of pore fluids in forearc sediments from Costa Rica (ODP Leg 170) [J]. Marine Geology, 2000, 167 : 1-28.
  • 3Volgin A V,Woodside J M. Sidescan sonar images of mud volcanoes from the Mediterranean Ridge[J]. Marine Geology, 1996,132 : 39-53.
  • 4Huguen C, Masclea J, Chaumillon E, et al. Structural setting and tectonic control of mud volcanoes from the Central Mediterranean Ridge (Eastern Mediterranean) [J]. Marine Geology, 2004,209 : 245-263.
  • 5Kopf A,Robertson A H F,Clennell M B,et al. Mechanisms of mud extrusion on the Mediterranean Ridge Accretionary Complex[J]. Geo-Marine Letters. 1998, 18:97-114.
  • 6Roy K O L, Sibueta M, Fiala M A, et al. Cold seep communities in the deep eastern Mediterranean Sea: composition,symbiosis and spatial distribution on mud volcanoes[J]. Deep-Sea Research I , 2004, 51: 1915-1936.
  • 7Kopf A,Klaeschen D, Mascle J. Extreme efficiency of mud volcanism in dewatering accretionary prisms[J]. Earth and Planetary Science Letters, 2001, 189: 295- 313.
  • 8Charlou L,Donval J P,Zitter T. Evidence of methane venting and geochemistry of brines on mud volcanoes[J].Deep-Sea Research I ,2003,50:941-958.
  • 9Chaumillon E, Mascle J. From foreland to forearc domains: New multichannel seismic reflection survey of the Mediterranean ridge accretionary complex (Eastern Mediterranean) [J]. Marine Geology, 1997, 138: 237-259.
  • 10Greinert J,Bollwerk S M, Derkachev A, et al. Massive barite deposits and carbonate mineralization in the Derugin Basin,Sea of Okhotsk: precipitation processes at cold seep sites[J]. Earth and Planetary Science Letters,2002,203:165-180.

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