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| 1 | ^(40)Ar/^(39)Ar age evidence for Altyn fault tectonic activities in western China显示文摘Four 40Ar/39Ar age groups of mica, hornblende and K-feldspar were obtained from Proterozoic and early Paleozoic metamorphic rocks in the Aksay-Dangjin Pass area, western China. The samples away from the middle shear zone of the Altyn fault belt yield two plateau age groups in the range of 461—445.2 Ma and 414.9—342.8 Ma, respec-tively. They represent the tectono-thermal events that had been recorded in the rocks that were displaced by the Altyn strike-slip fault in late Ordovician-early Silurian and Devo-nian, respectively. These two age groups should be related to the closures of Northern and Southern Qilian Oceans. The deformed granitic gneiss from the northern belt gives a pla-teau age group of 178.4—137.5 Ma, which is interpreted as the active age of the Altyn fault in the middle-late Jurassic- early Cretaceous and should be related to the accretion of Lhasa block to the north. The sample from the middle shear zone of the Altyn fault belt yields two plateau ages of 36.4 and 26.3 Ma, respectively, suggesting the strike-slip move-ment with strong metamorphism at greenschist facies along the Altyn fault in the late Eocene. This event occurred in the most areas of the northern Tibet Plateau and should be in response in the north to the collision between Indian and Eurasian continents. The present study demonstrates that the Altyn fault is characterized by multiple pulse-style activi-ties under the tectonic setting of convergence between the Indian and Eurasian continents. | LIU Yongjiang1, J. Genser2, GE Xiaohong1, F. Neubauer2, G. Friedl2, CHANG Lihua1, REN Shoumai3 & R. Handler2 1. College of Earth Sciences, Jilin University, Changchun 130061, China 2. Institute of Geology and Paleontology, Salzburg University, Salzburg A-5020, Austrilia 3. Statigraphic Research Center for Oil and Natural Gas, Ministry of Land and Resources, Beijing 100034, China Correspondence should be addressed to Liu Yongjiang (e-mail: liuyj@ email.jlu.edu.cn) | 2003 | Chinese Science Bulletin2003，48，18： | 28 |
| 2 | Laser probe ^(40)Ar/^(39)Ar dating of mica on the deformed rocks from Altyn Fault and its tectonic implications,western China显示文摘The samples of Caledonian mylonitized granite and Jurassic meta-sedimentary rocks were collected in the north of Dangjinshan Pass, Qaidam gate fault-valley and Gesi fault-valley. Detailed studies under the microscope and electronic microscope suggest that all the samples contain the syntectonic-growing minerals such as white mica, chlorite, sericite, biotite, etc. By dating these minerals, we got a group of 40Ar/39Ar laser probe isochronal ages of 89-92 Ma and apparent ages of (46.6±6.4) Ma. The ages ranging from 97 to 46 Ma were reported for the first time in the isotopic dating researches of the Altyn Fault The isochronal age group of (98-89) Ma indicates that a ductile strike-slip event, with low-grade metamorphism, began in late Cretaceous. This suggests that the strike-slip movement of the Altyn Fault should be related to the formation of the so-called west tectonic syntaxis in the Nepal-western Kunlun area. | LIU Yongjiang, YE Huiwen, GE Xiaohong, CHEN Wen, LIU Junlai, REN Shoumai & PAN HongxunCollege of Earth Sciences, Changchun University of Science and Technology, Changchun 130061, China Graduate School, China University of Geosciences, Beijing 100083, China Laboratory of Isotopic Geochronology, Institute of Geology, Ministry of Land and Resources of China, Beijing 100037, China | 2001 | Chinese Science Bulletin2001，46，4： | 16 |
| 3 | MiR-181a-5p regulates 3T3-L1 cell adipogenesis by targeting Smad7 and Tcf7I2显示文摘 | Dan Ouyang Lifeng Xu Lihua zhang Dongguang Guo Xiaotong Tan Xiaofang Yu Junjie Qi Yaqiong Ye Qihong Liu Yongjiang Ma Yugu Li | 2016 | Acta Biochimica et Biophysica Sinica2016，48，11： | 9 |
| 4 | Stratification of metamorphic belts and its genesis in the Liaohe Group显示文摘Stratification of metamorphic belt in the Liaohe Group during M2 episode of the Lüliang metamorphic period is proposed. Its genesis is elucidated to be caused by bedding-parallel sliding, magma layered-intrussion and burial depth. | Sanzhong Li Zhensheng Yang Yongjiang Liu | 1998 | Chinese Science Bulletin1998，43，5： | 7 |
| 5 | Characteristics,timing,and offsets of the middle-southern segment of the western boundary strike-slip fault of the Songliao Basin in Northeast China显示文摘作为 Songliao 盆和 Da Hinggan 山的东方边缘的西方边界差错, Nenjiang-Balihan 差错位于东北中国的中央部分。是一个巨大的深层的 NNE 惹人注目的差错传统地被认为,由一个正常差错或分开差错排水量描绘了。域调查导致了发现可锻砍在 Lingxia 和 Louzidian 区域,中间和差错系统的南部的扇区的地区。作者在这个领域里进行了结构的元素的大小,微结构研究,有限紧张大小,石英的比较喜欢的水晶取向上的研究用电子背决定了散布使变形的岩石的衍射和白云母 40Ar/39Ar 年表在可锻砍地区。变丑 Lingxia 和 Louzidian 展示的结果表演可锻砍地区是类似的,并且他们代表一个连续差错,即, Nenjiang-Balihan 的中间南部的片断指责在早白垩纪(130 妈) 的可锻的砍,它经历了左首的罢工滑倒。由在 Nenjiang-Balihan 差错的双方上测量 Xar 蠢人河缝术和 Wolegen 组的排水量,差错的累积罢工滑倒偏移量是大约 4050 km,这被发现。 | HAN GuoQing LIU YongJiang Franz NEUBAUER Johann GENSER ZOU YunXin LI Wei LIANG ChenYue | 2012 | Science China Earth Sciences2012，55，3： | 7 |
| 6 | Blueschist from the Toudaoqiao Area, Inner Mongolia, NE China: Evidence for the Suture between the Ergun and the Xing'an Blocks显示文摘Blueschist accompanied by pelitic schist expose along the Xinlin-Xiguitu fault in the Toudaoqiao area, northeastern China. In this paper, the blueschist is systematically studied on the petrography and mineral chemistry. The amphiboles in the blueschist are zoned from winchite core to magnesioriebeckite/glaucophane rim to winchite outermost rim. The peak metamorphic conditions are defined by the mineral assemblage of magnesioriebeckite/glaucophane, epidote, high-Si phengite(Si<7.1), chlorite, albite, hematite and quartz, indicating an epidote-blueschist facies metamorphism. The P-T conditions are estimated as T=350–400 ℃ and P=10-12 kbar. The occurrence of the blueschist along the Xinlin-Xiguitu fault strongly suggests the fault is the suture between the Ergun and the Xing'an blocks situated in the eastern portions of the Central Asia Orogenic Belt(CAOB). | Limin Zhao Akira Takasu Yongjiang Liu Weimin Li | 2017 | Journal of Earth Science2017，28，2： | 5 |
| 7 | The enhanced corrosion resistance of UMAO coatings on Mg by silane treatment显示文摘The surface silanization was carried out on ultrasonic micro-arc oxidation(UMAO) coatings on pure magnesium using KH550 as silane coupling agent(SCA). The surface morphology, chemical bonds and corrosion resistance of the silane films were investigated by scanning electron microscope(SEM), Fourier transform infrared spectroscopy(FTIR) and electrochemical workstation, respectively. The results showed that hybrid coatings were successfully prepared on pure magnesium by UMAO-Na OH(1 mol/L, 2 mol/L, 3 mol/L)-SCA processing. The organic films with Si–O–Mg bonds are helpful for the reduction of the pores in UMAO coatings. The pores decreased with increasing Na OH concentration. Compared with single UMAO treatment, the corrosion potentials(Ecorr) of magnesium plates with UMAO-Na OH(1 mol/L,2 mol/L, 3 mol/L)-SCA treatment increased by 29 m V, 53 m V and 75 m V, respectively, meanwhile the corrosion current density(Icorr) reduced one to two orders of magnitude. It indicated that the corrosion resistance of the coatings was improved by silane treatment. | Muqin Li Jiang Liu Jungang Li Yongjiang Li Shouduo Lu Yuqi Yuan | 2014 | Progress in Natural Science:Materials International2014，24，5： | 4 |
| 8 | Microbiota characteristics in Sebastes schlegelii intestine in early life stages显示文摘The structure of intestinal microbiota of black rockfish Sebastes schlegelii in five early development stages were determined in high throughput sequencing with Illumina MiSeq PE300 system.The relationship between intestinal microbial community and the environmental(including culture water and feed)microbiota and the abundance variation trends of core microbiota were investigated,based on which the source of some core microbiota was analyzed in this study.The results show that Proteobacteria and Firmicutes are the most dominant phyla in guts.At the genus level,there are obvious differences between the artificial breeding fish and wild adults in the intestinal microflora structure.The compositions of dominant genera are similar,although the structure of intestinal microbiota gradually changes with the growth of larvae and juveniles.The core microbiota including Bacillus,Acinetobacter,Pseudomonas,Lactobacillus,Lactococcus,Glaciecola,Vibrio,Pseudoalteromonas,Acidovorax,and Aliivibrio were determined in the analysis of dominant and shared species.Compared with the water,the effect of feed microbiota on the structure of the gut microbial community is more obvious.Moreover,the trends of Bacillus,Acinetobacter,Pseudomonas,Lactobacillus,Lactococcus,and Glaciecola were opposite to Vibrio and Pseudoalteromonas in the gut.The correlation analysis suggested that Acidovorax,Glaciecola,Pseudomonas,Lactobacillus,and Acinetobacter might transited from mainly the parents and/or came from the fertilization process.The relative results may provide a theoretical reference for selecting the native probiotics,and supply the basic data for artificially regulating the intestinal microbiota with probiotic during early developmental stage of black rockfish. | JIANG Yan LIU Xuezhou XU Yongjiang SHI Bao WANG Bin | 2020 | Journal of Oceanology and Limnology2020，38，1： | 3 |
| 9 | Zn-Rich Spinel in Association with Quartz in the Al-Rich Metapelites from the Mashan Khondalite Series, NE China显示文摘Al-rich metapelites from the Mashan khondalite series are characterized by the assemblage Spl+Grt+Sil+Crd+Bt+Pl(An72)+Kfs+Quartz+graphite. Large amounts of spinel+quartz assemblages occur as inclusions in garnet and prismatic sillimanite in the Al-rich metapelites of the Mashan complex, NE China. The chemical composition of spinel is characterized by Zn-rich(XZn=0.33–0.40. XZn=Zn/Zn+Mg+Fe*)(Fe*=Fe2++Fe3+) and Fe3+ rich(up to 0.31 p.f.u.). The characteristic chemical composition and the mineral association indicated that the formation of spinel and quartz assemblage may be due to the breakdown of Zn-rich staurolite. The geothermobarometers studies show that the peak temperature of the Mashan complex is around 820 ℃ and the peak pressures is 8.0 kbar. The Mashan complex shows a typical orogen style P-T path. | Xinzhuan Guo Akira Takasu Yongjiang Liu Weimin Li | 2014 | Journal of Earth Science2014，25，2： | 3 |
| 10 | MicroRNA-181a-5p enhances cell proliferation in medullary thymic epithelial cells via regulating TGF-β signaling显示文摘在从不同年龄的老鼠的胸腺纸巾的 miRNAs 的表示侧面在我们的以前的学习被表明了。在 miRNA 表达式侧面的综合分析以后,我们证明 miR-181a-5p 的表达式显著地在 thymic 被减少从 10- 的上皮的房间(侦探) 到 19-month-old 鼠标当与那相比在从 1-month-old 的侦探由量的反向的 transcriptase 聚合酶的鼠标锁住反应时。我们在侦探假设了那 miR-181a-5p 可能通过调整一些基因或发信号的小径与年龄相关的胸腺复杂物被联系。测试这个假设,老鼠髓的 thymic 上皮的房间(MTEC1 ) 被使用。有 miR-181a-5p 的 Transfection 模仿支持了 MTEC1 房间的增长,但是没影响 apoptosis。效果被颠倒 miR-181a-5p 的表示什么时候在 MTEC1 房间被压制。而且,转变生长因素贝它受体(Tgfbr1 ) 我被酶试金作为 miR-181a-5p 的一个直接目标证实。而且,它被发现 miR-181a-5p 的那 overexpression 下面调整 Smad3 的 phosphorylation 并且堵住了发信号的转变生长因素贝它的激活。不过,一相反地,关联在 Tgfbr1 的表示之间被观察,在侦探的 miR-181a-5p 源于不同年龄的老鼠。一起,我们提供 miR-181a-5p 可以是在侦探,和表示的增长的一个重要内长的管理者的证据在侦探的 miR-181a-5p 的层次可以与年龄相关的胸腺复杂物被联系。 | Dongguang Guo Yaqiong Ye Junjie Qi Lihua Zhang Lifeng Xu Xiaotong Tan Xiaofang Yu Qihong Liu Jilong Liu Yuan Zhang Yongjiang Ma Yugu Li | 2016 | Acta Biochimica et Biophysica Sinica2016，48，9： | 2 |
| 11 | Convergence History of the Songliao and Jiamusi Blocks in the Eastern End of Central Asian Orogenic Belt: Evidence from Detrital Zircons of Late Paleozoic Sedimentary Rocks显示文摘Central Asian Orogenic Belt(CAOB) is one of the largest accretionary orogenic belts in the world. The eastern segment of CAOB is dominated by Paleozoic Paleo Asian Ocean tectonic regime, Mesozoic Paleo-Pacific tectonic regime and Mongolian-Okhotsk tectonic regime. The Songliao and Jiamusi blocks are located in the easternmost part of the CAOB and are the key region to solve the problem about overprinting processes of multiple tectonic regimes. It is generally believed that the Mudanjiang Ocean between the two blocks was finally closed in the Mesozoic, but the Paleozoic magmatism also developed along the Mudanjiang suture zone, while on both sides of the suture zone, there were comparable Paleozoic strata, indicating that the two blocks had converged during the Paleozoic, and the evolution history of the two blocks in the Late Paleozoic remains controversial. The Carboniferous-Permian terrestrial strata mainly developed in Binxian, Wuchang and Tieli on Songliao Block, Baoqing and Mishan on Jiamusi Block. Samples from the Songliao and Jiamusi blocks in the Late Carboniferous-Early Permian and Late Permian are collected for comparative analysis. The LAICP-MS zircon U-Pb dating results show that the maximum depositional age of Middle Permian Tumenling Formation and Late Permian Hongshan Formation in Songliao Block is ~260 Ma, while that of Tatouhe Formation and Carboniferous strata in Jiamusi Block are ~290 Ma and ~300 Ma, respectively, which supports the previous stratigraphic division scheme. The age peaks of ~290-300 Ma, ~400 Ma, ~500 Ma appeared in the Late Carboniferous to Early Permian strata of Jiamusi Block and the Middle Permian strata of Songliao Block. The age peak of ~500 Ma in the Middle Permian strata of Songliao Block may come from the Cambrian basement, Mashan Complex, of Jiamusi Block, while the age peaks of ~420-440 Ma in the Carboniferous strata of Jiamusi Block may come from the Silurian magmatic arc in Zhangguangcai Range in the eastern margin of Songliao Block, reflects the history that they had been potential sources of each other, indicating that they may have combined in the Paleozoic. The Hongshan Formation of Songliao Block in the Late Permian lacks the age peak of ~500 Ma, which indicate that Jiamusi Block was not the provenance of Songliao Block in the Late Permian, that is, there was a palaeogeographic isolation between the two blocks. Combined with the ~210 Ma bimodal volcanic rocks developed along the Mudanjiang suture zone reported previously, we believe that the oceanic basin between the Songliao and Jiamusi blocks should have been connected in Late Permian and reopened during Late Permian to Late Triassic. | CHEN Zhaoxu LIU Yongjiang GUAN Qingbin | 2019 | Acta Geologica Sinica(English Edition)2019，93，5： | 2 |
| 12 | Final Closure Time of the Paleo-Asian Ocean: Implication from the Provenance Transformation from the Yangjiagou Formation to Lujiatun Formation in the Jiutai Area, NE China显示文摘The Jiutai area is tectonically situated at the eastern segment of the Central Asian Orogenic Belt(CAOB) and is close to the North China Craton(NCC) to the south, serving as an ideal place to investigations of the closure of the PaleoAsian Ocean(PAO). Sandstone samples collected from the Yangjiagou Formation and the Lujiatun Formation in this area have been studied in detail in terms of petrology, geochronology and geochemistry. The maximum depositional time of the Yangjiagou and Lujiatun formations has been constrained to early Middle Triassic(ca. 245 Ma) and middle Late Triassic(ca. 219 Ma), respectively. The Yangjiagou Formation, with a major provenance of dissected island arcs, is dominantly composed of Phanerozoic sediments from Northeastern China(NE China) massifs. The Lujiatun Formation, with major sediments from active continental margins, has a relatively larger proportion of Precambrian sediments, in which the ~1.85 Ga and ~2.5 Ga sediments are typical of the crystalline basements of the NCC and NE China massifs, which were uplifted and eroded during the closure of the PAO. Besides, both formations show the enrichment in LREEs and the depletion in HREEs, the common Eu negative anomalies, and trace element contents similar to that of the upper continental crust. Based on the provenance analysis of these two formations, the final closure time of the PAO in this area is constrained as from the early Middle Triassic(ca. 245 Ma) to the middle Late Triassic(ca. 219 Ma). | ZHANG Qian LIANG Chenyue LIU Yongjiang ZHENG Changqing LI Weimin | 2019 | Acta Geologica Sinica(English Edition)2019，93，5： | 2 |
| 13 | Bacterial outer membrane vesicles-based therapeutic platform eradicates triple-negative breast tumor by combinational photodynamic/chemo-/immunotherapy显示文摘Bacterial outer membrane vesicles(OMVs)are potent immuno-stimulating agents and have the potentials to be bioengineered as platforms for antitumor nanomedicine.In this study,OMVs are demonstrated as promising antitumor therapeutics.OMVs can lead to beneficial M2-to-M1 polarization of macrophages and induce pyroptosis to enhance antitumor immunity,but the therapeutic window of OMVs is narrow for its toxicity.We propose a bioengineering strategy to enhance the tumor-targeting ability of OMVs by macrophage-mediated delivery and improve the antitumor efficacy by co-loading of photosensitizer chlorin e6(Ce6)and chemotherapeutic drug doxorubicin(DOX)into OMVs as a therapeutic platform.We demonstrate that systemic injection of the DOX/Ce6-OMVs@M therapeutic platform,providing combinational photodynamic/chemo-/immunotherapy,eradicates triple-negative breast tumors in mice without side effects.Importantly,this strategy also effectively prevents tumor metastasis to the lung.This OMVs-based strategy with bioengineering may serve as a powerful therapeutic platform for a synergic antitumor therapy. | Yongjiang Li Junyong Wu Xiaohan Qiu Suhe Dong Jun He Jihua Liu Wenjie Xu Si Huang Xiongbin Hu Da-Xiong Xiang | 2023 | Bioactive Materials2023，，2： | 2 |
| 14 | The analysis of genetic diversity and differentiation of six Chinese cattle populations using microsatellite markers显示文摘A total of 321 individuals from six cattle populations of four species in a bovine subfamily in China were studied using 12 pairs of mi- crosatellite markers. The genetic diversities within and between populations were calculated. The phylogenetic trees were constructed by (δμ) 2 and DA distances, and the divergence times between populations were estimated by (δμ) 2. Altogether, 144 microsatellite alleles were detected including 24 private alleles and nine shared alleles. Chinese Holstein had the largest number of private alleles (10), whereas, Bohai black and Buffalo had the smallest number of private alleles (2). Chinese Holstein showed the highest genetic variability. Its ob- served number of alleles (Na), mean effective number of alleles (MNA), and mean heterozygosity (He) were 7.7500, 4.9722, and 0.7719, respectively, whereas, the Buffalo and Yak showed low genetic variability. In the phylogenetic trees, Luxi and Holstein grouped first, followed by Bohai and Minnan. Yak branched next and buffalo emerged as the most divergent population from other cattle populations. Luxi and Bohai were estimated to have diverged 0.039-0.105 million years ago (MYA), however, buffalo and Holstein diverged 0.501-1.337 MYA. The divergence time of Yak versus Minnan, Holstein and buffalo was 0.136-0.363, 0.273-0.729, and 0.326-0.600 MYA, respectively. | Yongjiang Mao Hong Chang Zhangping Yang Liu Zhang Ming Xu Guobin Chang Wei Sun Guangming Song Dejun Ji | 2008 | Journal of Genetics and Genomics2008，35，1： | 2 |
| 15 | An Early Stage Faulting Along the Altun Mountain Range——Microstructural Evidences显示文摘Structural, microstructural analysis is done on the Altun fault zo ne and fault rocks. The major characteristics of faulting are summarized. Micros tructural observation reveals a complicated evolution of the fault zone. Much at tention is paid to the microstructural observation and dynamic analysis of fault ing. The occurrence of phengite grains suggest abnormally high pressure conditio ns during ductile deformation and metamorphism, while the occurrence of muscovit e-chlorite mineral assemblage suggest a low temperature and low pressure condit i on. Micro-component analysis on the inter-grown muscovite and chlorite grains gives similar information. It is concluded that the first deformation along the Altun fault zone is a type of ductile shearing, forming mylonites and mylonitic rocks along the fault zone. A post-Jurassic deformation is primarily suggested by the involvement of the l atest tectonic units (Jurassic) in the ductile deformation.The early tectonic ev ent involves deformation and metamorphism under conditions in the upper crust, w ith T-P conditions varying to a large extent (T-270℃ ~350℃; P-0.005GPa~0. 43GPa), which may be attributed to the extra tectonic stresses. | Liu Junlai, Pan Hongxun, Ye Huiwen, Ge Xiaohong and Liu Yongjiang (Changchun Univ. Sci & Tech., 130026, Changchun, China) | 1999 | Global Geology1999，4，2： | 2 |
| 16 | Precambrian crustal evolution in Rangrim Massif,Korean Peninsula显示文摘Petrological,chronological and geotectonic geological analysis of Precambrian metamorphic rock in Korean Peninsula shows that the remnants(>3.4 Ga) of continental nuclei crust were formed in the Paleoarchean in the Rangrim Massif.In the massif,the main formation ages of continental crust range from 3.2 Ga to 2.5 Ga,its important growing period was 2.8-2.5 Ga.The subsequent expansion period of the Rangrim Massif was 2.4-2.2 Ga.The division events occurred in 1.85 Ga and in the Late Paleoproterozoic--Early Mesopro-terozoic,respectively.Since then the massif was relatively stable.However,the last division of the Rangrim Massif occurred at 793 Ma. | LYANG To Jun LIU Yongjiang YANG Jong Hyok KIM Hon HAN Ryong Yon KIM Jong Nam | 2009 | Global Geology2009，12，2： | 2 |
| 17 | Abrupt uplift of Tibetan Plateau at the end of early Pleistocene and Australasian impact event显示文摘The latest sharp uplift of the Tibetan Plateau and adjacent mountains occurred at the end of the early Pleistocene. The uplift of the Plateau resulted from Late Mesozoic--Cenozoic compressional structure due to the subduction of the Indian Plate beneath the Asian continent. This event definitively effected the formation of basin-mountain relief, Cenozoic basin deformation, large scale aridity and desertification of western China. The Australasian meteorites impact event happened ca. 0.8 Ma ago, located in the triangle area of the Indian Ocean ridge (20°S/67°E). The impact may have resulted in an acceleration of speeding of the Indian Ocean ridge pushing the Indian Plate to subduct rapidly northward. Thus, the impact event can give reasonable explanation for the dynamic background of the latest rapid uplift of the Tibetan Plateau and the continental deformation of western China and even of the Middle Asia. | REN Shoumai LIU Yongjiang GE Xiaohong | 2009 | Global Geology2009，12，3： | 2 |
| 18 | Gird manufacturing: A new solution for cross -enterprise collaboration 显示文摘 | QIONG LIU YONGJIANG SHI | 2008 | International Journal Advanced Manufacturing Technology2008，36，： | 1 |
| 19 | Genesis of lower strain S-L-type tectonitesin Daqingshan area, Inner Mongolia显示文摘Usual ductile shear zone has relatively high strain magnitude. However,for high-grade metamorphic rocks in Daqingshan area,the related strain is very low with weakly developed lineation. Significantly,the finite strain type with a K-value slightly lower than 1 and is characterized by compressional strain. Because the special tectonic environment with high temperature,the percentage of melt is relatively higher,which leads to a series of microscopic phenomenon such as multi-grain quartz bands,feldspar three edges equilibrium-like texture,granular flow,etc. As a consequence,the tectonites in the studied area illustrate a unique character: obvious rheological meso-deformation structure but with very weak intracrystalline micro-deformation. | SHAO Yilun LIU Yongjiang JIA Jie LI Weimin JIN Wei | 2016 | Global Geology2016，19，2： | 1 |
| 20 | Prediction of moisture variation during composting process: A comparison of mathematical models显示文摘 | Yongjiang Wang Ping Ai Hongliang Cao Zhigang Liu | 2015 | Bioresource Technology2015，，： | 1 |
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