Matches in SemOpenAlex for { <https://semopenalex.org/work/W2953018453> ?p ?o ?g. }
- W2953018453 endingPage "354" @default.
- W2953018453 startingPage "354" @default.
- W2953018453 abstract "Until recently, the characteristics of nano-microscale structures in the naturally deformed, overmature, marine shales were poorly known. Thermally overmature Lujiaping shales in the complex tectonic area of the northeast part of the upper Yangtze area, China have experienced strong tectonic deformation and are considered as potentially important strata for shale gas exploration. Naturally deformed samples from the main source rocks are selected from the Lower Cambrian Lujiaping Formation in the Dabashan Thrust-fold Belt to investigate nanometer- to micrometer-sized structures. A combination of scanning electron microscope (SEM), low-pressure nitrogen adsorption (LPNA), and low-field nuclear magnetic resonance (NMR) suggests that the pore types are dominantly fracture-related pores with a lesser abundance of mineral-hosted pores. These two pore types account for the 90% of total pore space. Organic matter (OM)-hosted pores are rare and make up a small part of the pore systems (less than 10%) due to high thermal maturity and intensive tectonic compression. Overall, the Lujiaping deformed, overmature samples have abundant nanometer- to micrometer-sized inorganic pores. High-resolution SEM images provide direct evidence of the formation of nano- and microsized structures such as OM–clay aggregates and silica nanograins. OM–clay aggregates are commonly observed in samples, which also exhibit abundant open microfractures and interparticle pores. Quartz can occur as silica nanograins and botryoids typically 20–100 nm in size, which may influence porosity through the creation or occupying interparticle pore space." @default.
- W2953018453 created "2019-06-27" @default.
- W2953018453 creator A5016590889 @default.
- W2953018453 creator A5018819770 @default.
- W2953018453 creator A5028521547 @default.
- W2953018453 creator A5033698454 @default.
- W2953018453 creator A5037023585 @default.
- W2953018453 creator A5070802812 @default.
- W2953018453 creator A5075771580 @default.
- W2953018453 creator A5078494464 @default.
- W2953018453 creator A5085624718 @default.
- W2953018453 creator A5090481419 @default.
- W2953018453 date "2019-06-10" @default.
- W2953018453 modified "2023-10-06" @default.
- W2953018453 title "Tectonic and Thermal Controls on the Nano-Micro Structural Characteristic in a Cambrian Organic-Rich Shale" @default.
- W2953018453 cites W1515271349 @default.
- W2953018453 cites W1970155529 @default.
- W2953018453 cites W1970393795 @default.
- W2953018453 cites W1977275561 @default.
- W2953018453 cites W1979044833 @default.
- W2953018453 cites W1980073009 @default.
- W2953018453 cites W1980083955 @default.
- W2953018453 cites W1982168155 @default.
- W2953018453 cites W1983187325 @default.
- W2953018453 cites W1998396889 @default.
- W2953018453 cites W2013591344 @default.
- W2953018453 cites W2045518543 @default.
- W2953018453 cites W2071771565 @default.
- W2953018453 cites W2074401251 @default.
- W2953018453 cites W2074579280 @default.
- W2953018453 cites W2084196175 @default.
- W2953018453 cites W2104447116 @default.
- W2953018453 cites W2134189468 @default.
- W2953018453 cites W2134744054 @default.
- W2953018453 cites W2135535608 @default.
- W2953018453 cites W2140460370 @default.
- W2953018453 cites W2140962967 @default.
- W2953018453 cites W2150922969 @default.
- W2953018453 cites W2156608310 @default.
- W2953018453 cites W2158897778 @default.
- W2953018453 cites W2168621338 @default.
- W2953018453 cites W2182263886 @default.
- W2953018453 cites W2197251011 @default.
- W2953018453 cites W2326312167 @default.
- W2953018453 cites W2339191110 @default.
- W2953018453 cites W2395256810 @default.
- W2953018453 cites W2466533673 @default.
- W2953018453 cites W2512684499 @default.
- W2953018453 cites W2520504205 @default.
- W2953018453 cites W2521407017 @default.
- W2953018453 cites W2590672111 @default.
- W2953018453 cites W2624747578 @default.
- W2953018453 cites W2626339562 @default.
- W2953018453 cites W2626523792 @default.
- W2953018453 cites W2626638488 @default.
- W2953018453 cites W2756897547 @default.
- W2953018453 cites W2761147696 @default.
- W2953018453 cites W2762216730 @default.
- W2953018453 cites W2767354513 @default.
- W2953018453 cites W2781742221 @default.
- W2953018453 cites W2792429958 @default.
- W2953018453 cites W2792596522 @default.
- W2953018453 cites W2799635136 @default.
- W2953018453 cites W2801218484 @default.
- W2953018453 cites W2802529188 @default.
- W2953018453 cites W2804355587 @default.
- W2953018453 cites W2883545228 @default.
- W2953018453 cites W2891687895 @default.
- W2953018453 cites W2900261890 @default.
- W2953018453 cites W2905799587 @default.
- W2953018453 cites W2908058440 @default.
- W2953018453 cites W2908159043 @default.
- W2953018453 cites W2911726443 @default.
- W2953018453 cites W2913680554 @default.
- W2953018453 cites W2916280800 @default.
- W2953018453 cites W2917904272 @default.
- W2953018453 doi "https://doi.org/10.3390/min9060354" @default.
- W2953018453 hasPublicationYear "2019" @default.
- W2953018453 type Work @default.
- W2953018453 sameAs 2953018453 @default.
- W2953018453 citedByCount "13" @default.
- W2953018453 countsByYear W29530184532019 @default.
- W2953018453 countsByYear W29530184532020 @default.
- W2953018453 countsByYear W29530184532021 @default.
- W2953018453 countsByYear W29530184532022 @default.
- W2953018453 countsByYear W29530184532023 @default.
- W2953018453 crossrefType "journal-article" @default.
- W2953018453 hasAuthorship W2953018453A5016590889 @default.
- W2953018453 hasAuthorship W2953018453A5018819770 @default.
- W2953018453 hasAuthorship W2953018453A5028521547 @default.
- W2953018453 hasAuthorship W2953018453A5033698454 @default.
- W2953018453 hasAuthorship W2953018453A5037023585 @default.
- W2953018453 hasAuthorship W2953018453A5070802812 @default.
- W2953018453 hasAuthorship W2953018453A5075771580 @default.
- W2953018453 hasAuthorship W2953018453A5078494464 @default.
- W2953018453 hasAuthorship W2953018453A5085624718 @default.
- W2953018453 hasAuthorship W2953018453A5090481419 @default.
- W2953018453 hasBestOaLocation W29530184531 @default.