震积岩的特征、成因与浊积岩比较
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摘要
震积岩是在地层中具有古地震事件纪录的一类岩石的总称。震积岩和浊积岩都是属于事件性沉积范畴,其起因于一定的触发机制,阵发性因素直接或间接诱发下而形成。震积岩是由地震作用所产生的具有震积构造和震积岩序列的灾变事件沉积的。广义上说浊积岩就是由浊流沉积作用而形成的岩石组合。认清震积岩与浊积岩两者之间的相互区别和联系,这对于油气勘探也是很有指导意义的。
seismites are rocks as archives of ancient earthquake activities,which can supply the dynamics explanation for the crust evolution,It is to belong to incident sediment category to seismite and turbidite,its cause in certain trigger mechanism,clonic factor brings out directly or indirectly and forms.seismite is from seismic role produce have the calamity that shakes product structure and shakes product rock sequence change incident sediment.On broad sense say turbidite for is from turbid flow out the rock combination that sediment role forms.We have seen clearly to shake connection and the mutual difference between product rock and turbid product rock two,this also has guidance meaning very much for the exploration of oil gas.
seismites are rocks as archives of ancient earthquake activities,which can supply the dynamics explanation for the crust evolution,It is to belong to incident sediment category to seismite and turbidite,its cause in certain trigger mechanism,clonic factor brings out directly or indirectly and forms.seismite is from seismic role produce have the calamity that shakes product structure and shakes product rock sequence change incident sediment.On broad sense say turbidite for is from turbid flow out the rock combination that sediment role forms.We have seen clearly to shake connection and the mutual difference between product rock and turbid product rock two,this also has guidance meaning very much for the exploration of oil gas.
引文
[1]杜远生,韩欣.论海啸作用与海啸岩[J].地质科技情报,2000,(01).
[2]乔秀夫.中国震积岩的研究与展望[J].地质论评,1996,(04).
[3]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,(04).
[4]冉勇康,邓起东.古地震学研究的历史、现状和发展趋势[J].科学通报,1999,(01).
[5]张振晗,辛初波.沉积学研究的新进展与发展趋势[J].山西建筑,2006,(06).
[6]饶孟余,钟建华,赵志根,严家平,唐修义.浊流沉积研究综述和展望[J].煤田地质与勘探,2004,(06).
[7]李继亮,陈昌明,高文学,陈瑞君,黄家宽,田兴有,刘杰汉.我国几个地区浊积岩系的特征[J].地质科学,1978,(01).
[8]夏青松,田景春.浊积岩神话与砂质碎屑流[J].沉积与特提斯地质,2006,(04).
[9]Rossetti D F,Goes A M.Deciphering thesedimentologyical imprint of paleoseismicevents:an example from the Aptian Codoformation,northern Brazil.SedimentaryGeology.2000,135:137~156.
[10]Yeats R S.Introducton to speccial section:paleoseismology.J Geophy Res.1996,101(B3):5847~5853.
[11]Cowan H,Nicol A.A comparison ofhistorical and paleoseismicity in a newlyformed fault zone and a mature fault zine,North Canterbury,New Zealand.JgeophyRes.1996,101(B3):6021~6036.
[2]乔秀夫.中国震积岩的研究与展望[J].地质论评,1996,(04).
[3]杜远生,韩欣.论震积作用和震积岩[J].地球科学进展,2000,(04).
[4]冉勇康,邓起东.古地震学研究的历史、现状和发展趋势[J].科学通报,1999,(01).
[5]张振晗,辛初波.沉积学研究的新进展与发展趋势[J].山西建筑,2006,(06).
[6]饶孟余,钟建华,赵志根,严家平,唐修义.浊流沉积研究综述和展望[J].煤田地质与勘探,2004,(06).
[7]李继亮,陈昌明,高文学,陈瑞君,黄家宽,田兴有,刘杰汉.我国几个地区浊积岩系的特征[J].地质科学,1978,(01).
[8]夏青松,田景春.浊积岩神话与砂质碎屑流[J].沉积与特提斯地质,2006,(04).
[9]Rossetti D F,Goes A M.Deciphering thesedimentologyical imprint of paleoseismicevents:an example from the Aptian Codoformation,northern Brazil.SedimentaryGeology.2000,135:137~156.
[10]Yeats R S.Introducton to speccial section:paleoseismology.J Geophy Res.1996,101(B3):5847~5853.
[11]Cowan H,Nicol A.A comparison ofhistorical and paleoseismicity in a newlyformed fault zone and a mature fault zine,North Canterbury,New Zealand.JgeophyRes.1996,101(B3):6021~6036.
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