intraclast 中文意思是什麼
intraclast
解釋
內成碎屑灰巖-
Through the search of bourn of intraclast congeries silica rock, its earth and west side all grow consortium robble
經對內碎屑堆積硅質巖的邊界研究發現，其東西兩側均發育有同生斷裂。 -
Ore area locate on, silver factory ditch - ancient tomb ditch in west branch river set lower bench, stratigraphic succession, rock assemblage are different with circumference. most is a set of intraclast congeries silica rock. in search of it, its distribution range in the silver factory ditch - ancient tomb ditch
礦區所在部位銀廠溝?古墓溝一帶，西岔河組下段地層中，地層層序、巖石組合特徵與周邊地區存在明顯的差異。主要為一套內碎屑堆積的硅質巖。 -
Further research of lithofacies pvove : lode country output points belongs to tidal - flat facies. and the two sides belong to littoral facies - estuarine facies. ore area petrochemistry analyse also prove : intraclast congeries silica rock in basin have higher cu, ag abundance than circumference pena. the prominence inhomogeneity of the cu distribution indicates reconstruct of the late construction
礦區內巖石化學測量也證明：盆地內發育的內碎屑堆積硅質巖比周圍巖石具有更高的cu 、 ag元素地球化學豐度值， cu元素分佈的顯著不均一性，表明了後期構造的改造作用。 -
The microfacies characteristic of carbonate rock of suonahu formation in cuoqinin basin constitutes with the marl lithofacies, the intraclast ash lithofacies, biological detritus ash lithofacies
措勤盆地嗩吶湖組碳酸鹽巖微相由內碎屑灰巖相、生物碎屑灰巖相和泥灰巖相組成。 -
The northern qiangtang basin suonahu formation microfacies of carbonate rock is divided for the intraclast ash lithofacies, biological detritus ash lithofacies, oncolite limestone lithofacies, contain the calcium and alga ash lithofacies, marl lithofacies and pure microlite limestone lithofacies
羌北盆地嗩吶湖組碳酸鹽巖微相為內碎屑灰巖相、生物碎屑灰巖相、核形石灰巖相、含膏藻灰巖相、泥灰巖相和純微晶灰巖相等6種微相。 -
Synthesizely contrasted the suonahu formation profile of the northern qiangtang basin and cuoqin basin of miocene epoch, used the intraclast ash rock as the marker bed of the suonahu formation
對羌北盆地和措勤盆地中新世的嗩吶湖組剖面作了綜合對比，將內碎屑灰巖作為嗩吶湖組的標志層。 -
A lot of diagenetic dolostones have remainder granulation structure, and the native rock of it may be various intraclast limestone. this type of rock usually has high primary porosity. the high primary porosity is the important base of forming the pore of dolostone reservoir
一部分成巖白雲巖仍具有殘余粒屑結構，其原巖可能主要為各種類型的粒屑灰巖，這類巖石通常具有較高的初始孔隙度（原生孔隙度） ，這是以後形成成巖白雲巖儲層孔隙的重要基礎條件。
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