珊瑚灰岩构造
![珊瑚礁灰岩物性特征及工程性质研究进展建设21世纪海上丝绸之路](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A7314A62FDC94E0050081EF09549F4927971C7DE163052ABFF51A619B6C10482A640AF117FC9984EE1C77100220CE9397A3FC90742ECDD01BB1439D63461EF0D1C3572CDB3B651F8B876AE81A0CB4F18C9D)
珊瑚礁灰岩物性特征及工程性质研究进展建设21世纪海上丝绸之路
图片尺寸960x828![年09期图为一种常见管虫20米以上水深呈缓坡漏斗状永乐龙洞内珊瑚丛](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A738A249BF8ADE2313C02CAF3728F21ADA9066013F54FB89C0308D6EB08E757DCC98584E6E2DB9E68F7C83C87EE3983BE65E65F52FF7AFB21FE9971BFEFAA36E1D152A0061820A90EA2B7B45BF24CF4CA40)
年09期图为一种常见管虫20米以上水深呈缓坡漏斗状永乐龙洞内珊瑚丛
图片尺寸726x706![该地段三叠纪构造—岩浆活动强烈发育,以中酸性侵入岩体为主,形成许](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E90992995DBACD164F6E11053EF45C9060748BB2F86FCA1A4B0D34D981B9BCB607275A1E90BA7E355A86EEAB3E62EE9DD97C4B02AAFFD66F638BECFC7BE1FD2F2DACD407980B4ACE996275003F224970FE)
该地段三叠纪构造—岩浆活动强烈发育,以中酸性侵入岩体为主,形成许
图片尺寸1080x347![珊瑚礁灰岩孔隙网络结构量化表征研究获进展](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E939F5A1D4E0B4195DE9FF8EE6FAC967507ACCA3482DBBC8356F3CFD8623E26532B55361A75B28175098D313A3164E2814A89D0D1C1A7129D3AF1E101A911709B75C739EC44116D9A7CE483F15D735A69A)
珊瑚礁灰岩孔隙网络结构量化表征研究获进展
图片尺寸600x232![1,礁无论潮汐状况如何都露出水面的小块陆地,一般由岩石或珊瑚构成,但](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83DB41DBA206BE9CF565AC45C962652799B275AF12FEC0C3B1DAD76F8643E5C3BC8636759A0B810A2AB57DFEAEB5EF9BC472CC8538F96B28B2B7B49795835F5846AF81932706A3E15276E3813ACD22594B)
1,礁无论潮汐状况如何都露出水面的小块陆地,一般由岩石或珊瑚构成,但
图片尺寸1200x800![海百合灰岩(剖面)50海百合灰岩49白垩系砂岩48珊瑚灰岩47砾岩46砾岩45](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A731E0E26805C04C0F529EB78511D896012B79C7355BA7B4E094082F150C2BF05FDBB8FF72352136495A0AE38914D25EA4C2FA5941427B95912E728308F7A52FFFC502931EAD4047B9AC7AF8DE2C2C2B105)
海百合灰岩(剖面)50海百合灰岩49白垩系砂岩48珊瑚灰岩47砾岩46砾岩45
图片尺寸660x649![珊瑚藻泥晶灰岩](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9F4A1A44456FA29C956009F6D92714C40F810F521C546B74F60B29EE614CDECBF92108BED49EF72C950AD48A4D2932C862819725A3C54F393BEADB03623C4F2B935D0A7C9A76D247301BBA6CECB7F0374)
珊瑚藻泥晶灰岩
图片尺寸640x1067![2泥晶生物碎屑灰岩(11)](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83B9A737C1129AB0E7284BB87C6333E3AB9E8BD2B92F269EEDEA9C68A780CCB801F6BC2BEF5D690A2D39566B7FFA741ACC80CDF9B5EB3222AD1A55962BCEA6B54D4AD2D42DB7C380EA8D815B073E65799D)
2泥晶生物碎屑灰岩(11)
图片尺寸640x952![鹅銮鼻位于台湾最南端,园内珊瑚礁石灰岩地形遍布,巨礁林立,怪石嶙峋](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83F72A7A1E8D05A7A92A5AF2B2178E2E09D609EE8DEBF6A80C876A4D9E7AB950397598BEF74AD4A7C90CFEF01A56F5C85A19CC8E1D4672529E213C0E9B1BE7599FED6387E8F5863781E28C4A8F76A5F799)
鹅銮鼻位于台湾最南端,园内珊瑚礁石灰岩地形遍布,巨礁林立,怪石嶙峋
图片尺寸800x600![礁灰岩的抛光面和薄片. a) 珊瑚-串管海绵-微生物綁结岩抛光面.](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83016DEC5EEE73C69FBBB9E3283395BDDB89183427BF25D7FC599E920F72583808272A5B01931173C71A2ABF1D7591B1D1FA7E102DCFEA6DFB03A2A5B8A916B60A4791DEB74788E011E5AE0DBB6C01F68D)
礁灰岩的抛光面和薄片. a) 珊瑚-串管海绵-微生物綁结岩抛光面.
图片尺寸700x591![48珊瑚灰岩47砾岩46砾岩45砾岩44砾岩团块43沥青42无烟煤41燧石40燧](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E833BEA9D86D487024A1BDD2CA7A1C0F78C59465A9FCECBA3948AD5DC226EF97AC05F1669E1835B604577785058CFF234FFCAA9F7C2E16D714B690A9C1B0B913AB8D9E943801E46680B59D982F1F1E5F473)
48珊瑚灰岩47砾岩46砾岩45砾岩44砾岩团块43沥青42无烟煤41燧石40燧
图片尺寸660x660![巴基斯坦珊瑚灰岩](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9A86DE7389FC17F522D798681110D3622B011F5789D530EA8EF3ABFE8A7384768A3EE54F2B271F5FDB02BA3F12632CD51BAD0450E8853903024C4266D66E7F19403A07F7D46AE2FAA3ECD9AFF486566C7)
巴基斯坦珊瑚灰岩
图片尺寸700x776![灰岩珊瑚藻泥晶灰岩砂质燧石岩细砾岩砂质灰岩砂质复成分砾岩砂屑颗粒](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E95B00F0984EAFEF14B2D3BBDC2604DB2849F5AAF5BC5F7ABB287E9D276D70AD4230A7CD832CC9A0F4B9E91858186CEA08BD79DAAB002BC45531184DEBE5FE4164DD840CB3D2962EA3EC2278B4AD10016F)
灰岩珊瑚藻泥晶灰岩砂质燧石岩细砾岩砂质灰岩砂质复成分砾岩砂屑颗粒
图片尺寸640x573![在贵州东部的寒武纪地层里,是一种构造简单的底栖固着"原始海百合";在](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83BEB0B1DB7A880348476892DD1D129C3E1BE9F71924BFA86F15F4E7D5C8E351950B545642178B552AC34DCA54C3BB31E9D910A012C5869CA0747D5B09A73FCC0B9F287B2510AE8B12080466B367F4678F)
在贵州东部的寒武纪地层里,是一种构造简单的底栖固着"原始海百合";在
图片尺寸2832x2128![最原始的海百合出现在贵州东部的寒武纪地层里,是一种构造简单的底栖](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A7394370C58AF34278BC9ACA1DC0490A8B1AA0018ECCBECA53AD6F0288A2278C9E8CD2E8BA47C4E2095033D998CD62C242FC37A39BF26FA8B9B3728050C15F352AD2D0DA523B1B6668292C5DF8376AF2E9D)
最原始的海百合出现在贵州东部的寒武纪地层里,是一种构造简单的底栖
图片尺寸660x880![不同瘤状灰岩(c和d为宝塔灰岩)以及它们的形成模式(e和f,f显示的是](https://imgs.wantubizhi.com/img/735A5D1F980B52A636CC46F12F2D1A7374FFD28EAA8C4B6B1DBF5EDD974B4738F4B74C03A24967526293922221775B1213AC82120691DC37CCC7CF59826E4E6E158640F9B1333A21DDFA8B61D781C9F87FC8E8FD4980FEB5D79B6F0C36EC3000)
不同瘤状灰岩(c和d为宝塔灰岩)以及它们的形成模式(e和f,f显示的是
图片尺寸800x943![4)断裂构造岩石受应力作用而发生变形,当应力超过一定强度时,岩石便](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9084764CA80E563297883318EA9B6A45256C8547EDFCBFBF82ECD5EB49B29C5501738BDF3B3F340E8D797E668B83DD61452E4A1306646E78C57EF18938522856641526A1EACFF7A5D66CA1F863A27D80F)
4)断裂构造岩石受应力作用而发生变形,当应力超过一定强度时,岩石便
图片尺寸1250x688![石膏岩生物碎屑颗粒灰岩渗滤粉砂鲕粒颗粒灰岩珊瑚藻泥晶灰岩砂质燧石](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E83620829A4A87803D6877AE0BDC3F7DE705B7329D2BF260D927648957874E0A42C11E46A8CD0E52B6DB807B9544C718CD43C235364FC2C075DE5190583FC0557BDC44BC468F589AB4C3346D797CDB82A43)
石膏岩生物碎屑颗粒灰岩渗滤粉砂鲕粒颗粒灰岩珊瑚藻泥晶灰岩砂质燧石
图片尺寸596x592![灰岩油页岩硬石膏岩岩屑杂砂岩岩屑石英杂砂岩细晶白云岩蜓颗粒灰岩](https://imgs.wantubizhi.com/img/A1A61BAA66193547F3A6DD7D8EE527E9240117CEB5136CF61433EED84B21AC5C2B5F6A003D506D2885074635F4BCD2C0CE5BA53598A347A292FFD136B8C51EDF216E3C10C20AF5C93009DB0E96A770D2F6D927F9E1F93F92B8E9108921439D0F)
灰岩油页岩硬石膏岩岩屑杂砂岩岩屑石英杂砂岩细晶白云岩蜓颗粒灰岩
图片尺寸640x579![沉积学_碳酸盐岩3](https://imgs.wantubizhi.com/img/ADDA3C5D760C6828B77B505A29D43E8327ECE5481A67C9B133405D1BD034633FDEA04FA3302B8102EEB4E76B10428C5E9F225F8699A684C25654A0936029A0A4A97FDA1988605113EB7CCC23721A0E78B472C8D5E10C5408EB48D342A6490474)
沉积学_碳酸盐岩3
图片尺寸1080x810