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Journal articles on the topic 'Isocon'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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1

Verdiansyah, Okki. "PERUBAHAN UNSUR GEOKIMIA BATUAN HASIL ALTERASI HIDROTERMAL DI GUNUNG WUNGKAL, GODEAN, YOGYAKARTA." KURVATEK 1, no. 1 (2016): 9. http://dx.doi.org/10.33579/krvtk.v1i1.198.

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Daerah Godean merupakan daerah perbukitan yang terdiri dari batuan beku yang diikuti oleh adanya alterasi hidrotermal dan pelapukan batuan yang cukup intensif. Litologi daerah Gunung Wungkal terdiri dari Andesit dasitik sampai dasit hornblenda, yang teralterasi lemah (klorit-pirit ) sampai kaolinit-smektit kuat kemudian terlapukan. Perubahan batuan terlihat dari adaya perubahan mineral, massa, volume dan geokimia mineral yang selanjutnya dihitung dengan metode Isocon - Grant (1986, 2005). Kemiringan (slope) isocon diperoleh dari nilai unsur ‘immobile’ (Ga, Y, Dy, Tm, Th) sebesar 1.01. Geokimia

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2

Kozlov, Evgeniy N., and Ekaterina N. Fomina. "Mass balance of complementary metasomatic processes using isocon analysis." MethodsX 9 (2022): 101609. http://dx.doi.org/10.1016/j.mex.2021.101609.

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3

OLSEN, S. N., and J. A. GRANT. "Isocon analysis of migmatization in the Front Range, Colorado, USA." Journal of Metamorphic Geology 9, no. 2 (1991): 151–64. http://dx.doi.org/10.1111/j.1525-1314.1991.tb00511.x.

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4

Grant, James A. "Isocon analysis: A brief review of the method and applications." Physics and Chemistry of the Earth, Parts A/B/C 30, no. 17-18 (2005): 997–1004. http://dx.doi.org/10.1016/j.pce.2004.11.003.

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5

Kuwatani, Tatsu, Kenta Yoshida, Kenta Ueki, Ryosuke Oyanagi, Masaoki Uno, and Shotaro Akaho. "Sparse isocon analysis: A data-driven approach for material transfer estimation." Chemical Geology 532 (January 2020): 119345. http://dx.doi.org/10.1016/j.chemgeo.2019.119345.

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6

Grant, James A. "The isocon diagram; a simple solution to Gresens' equation for metasomatic alteration." Economic Geology 81, no. 8 (1986): 1976–82. http://dx.doi.org/10.2113/gsecongeo.81.8.1976.

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7

Baumgartner, Lukas P., and Sakiko N. Olsen. "A least-squares approach to mass transport calculations using the isocon method." Economic Geology 90, no. 5 (1995): 1261–70. http://dx.doi.org/10.2113/gsecongeo.90.5.1261.

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8

Hilchie, Luke, J. K. Russell, and Clifford R. Stanley. "Unification of Isocon and Pearce Element Ratio Techniques in the Quantification of Material Transfer." Economic Geology 113, no. 7 (2018): 1603–8. http://dx.doi.org/10.5382/econgeo.2018.4605.

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9

Kozak, P. M., and J. Watanabe. "Meteors with extreme beginning heights from observations with high-sensitivity super-isocon TV systems." Monthly Notices of the Royal Astronomical Society 497, no. 4 (2020): 5550–59. http://dx.doi.org/10.1093/mnras/staa2183.

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ABSTRACT Meteors with extremely high altitudes are considered. Parameters of seven meteors having anomalous beginning heights recorded with highly sensitive super-Isocon TV systems are presented. One 1993 Perseid meteor, one 2001 sporadic meteor and five meteors from the 2002 Leonid storm had beginning heights in the range 135–145 km. The sporadic meteor is used to demonstrate the methods of data processing and observation precision results. The original TV meteor images, photometric calibration curves and meteor light curve are shown. Light curves are shown for the Leonid shower meteors as we

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10

Okki, Verdiansyah. "Geochemical Correlation Between Mafic and Felsic Igneous Rock from Godean, Yogyakarta, Indonesia." International Journal of Geology and Earth Sciences 2, no. 4 (2016): 55–63. https://doi.org/10.5281/zenodo.1560821.

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Godean is a as a part of Miocene Southern Mountain magmatisme range that occur in Yogyakarta, Indonesia. Godean is a hilly morphology that compose from several type of igneous rock occurs that are andesite and microdiorite intrusion, dacite subvolcanics to lava, and the latest is basalt subvolcanic. That’s rock indicated there is completes differentiation of igneous rock in Godean, that's occurs as felsic rock to mafic rock that must have a correlation in between. This research was conduct from field geological mapping, petrographic analysis, and complete geochemistry. Geochemical co

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11

MUKHERJEE, P. K., and P. K. GUPTA. "Arbitrary scaling in ISOCON method of geochemical mass balance: An evaluation of the graphical approach." GEOCHEMICAL JOURNAL 42, no. 3 (2008): 247–53. http://dx.doi.org/10.2343/geochemj.42.247.

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12

Guo, S., K. Ye, Y. Chen, and J. B. Liu. "A NORMALIZATION SOLUTION TO MASS TRANSFER ILLUSTRATION OF MULTIPLE PROGRESSIVELY ALTERED SAMPLES USING THE ISOCON DIAGRAM." Economic Geology 104, no. 6 (2009): 881–86. http://dx.doi.org/10.2113/gsecongeo.104.6.881.

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13

Mrozek, Stephanie A., Zhaoshan Chang, Carl Spandler, Steve Windle, Cesar Raraz, and Alberto Paz. "Classifying Skarns and Quantifying Metasomatism at the Antamina Deposit, Peru: Insights from Whole-Rock Geochemistry." Economic Geology 115, no. 1 (2020): 177–88. http://dx.doi.org/10.5382/econgeo.4698.

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Abstract At the Antamina deposit, Peru, accurate classification of exoskarns and endoskarns can be problematic when textures are mottled. In this study, we use whole-rock geochemical compositions (62 elements) of 221 samples to differentiate texturally similar endoskarns and exoskarns by comparing their compositions to least altered precursors (wall rocks and intrusive rocks). We present a simple method for discriminating these skarn types using immobile element bivariate plots. The most effective discriminators partition endoskarn and exoskarn into distinct domains defined by the composition

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14

Tsikouras, Basilios, Kalliopi-Sofia Passa, Ioannis Iliopoulos, and Christos Katagas. "Microstructural Control on Perlite Expansibility and Geochemical Balance with a Novel Application of Isocon Analysis: An Example from Milos Island Perlite (Greece)." Minerals 6, no. 3 (2016): 80. http://dx.doi.org/10.3390/min6030080.

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15

Zhang, Wengao, Bo Wang, Yifei Tang, et al. "Hydrothermal Alteration and Element Migration Patterns in the Zhangjiawu Uranium Deposit, Northern Zhejiang Province, China." Minerals 13, no. 3 (2023): 335. http://dx.doi.org/10.3390/min13030335.

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The Zhangjiawu uranium deposit is the largest volcanic rock-type uranium deposit in the northern Zhejiang Province, China. The deposit has developed hydrothermal alteration, with obvious alternating zoning phenomena from the mineralized center to the fresh surrounding rocks. Based on detailed field and petrographic observations of typical ore bodies, the uranium mineralized section of the Zhangjiawu uranium deposit was divided into mineralized central, ore-side alteration, near-ore alteration and far-ore alteration zones, whose hydrothermal alteration intensity decreases sequentially. Using th

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Imamalipour, Ali, Samaneh Barak, and Farzaneh Mami Khalifani. "Quantifying mass changes during hydrothermal alteration in listwaenite-type mercury mineralization, Tavreh area, northwestern Iran." Geochemistry: Exploration, Environment, Analysis 20, no. 4 (2020): 425–39. http://dx.doi.org/10.1144/geochem2020-004.

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The Tavreh mercury prospect, a listwaenite-type alteration/mineralization system, is located c. 90 km west of Khoy in northwestern Iran. Tavreh is hosted within the Khoy ophiolite zone. Three types of listwaenites have been recognized in the Khoy ophiolite: silica, silica-carbonate and carbonate. Of these three, Hg mineralization at Tavreh is spatially and genetically associated with the silica-type listwaenite, also known as berberite. Alteration and mineralization at Tavreh are restricted to a faulted contact between shale and serpentinite. The Tavreh listwaenite is inferred to form from the

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17

Villareal-Tirona, Aubrey Marie, Maria Ines Rosana Balangue-Tarriela, and Ray Shaw. "Sulfidation And Gold Precipitation In The Jugan Gold Deposit In Bau, Sarawak, East Malaysia: Insights From Correlation Plots And Factor Analysis." Bulletin of the Geological Society of Malaysia 74, no. 1 (2022): 55–67. http://dx.doi.org/10.7186/bgsm74202204.

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The Jugan Gold Deposit (JGD) is part of the Bau Mineral District (BMD) in Bau, Sarawak, East Malaysia. Although the mineral district is well studied, limited studies were conducted on the JGD. This paper presents the results of statistical studies using the multi-element geochemical data emphasizing the trace elements association with gold, alteration-mineralization, and the precipitation mechanism of the gold-bearing sulfide minerals. The correlation matrix displays positive correlation associations, particularly those associated with gold mineralization, i.e., arsenic, sulfur, antimony, and

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18

Permatasari, A., W. A. S. Pratiwi, M. R. Parningotn, Ernowo, and S. Sitohang. "Elemental Mass Balance Calculation of the Hydrothermal Alteration in Awak Mas Gold Deposit, Sulawesi Island, Indonesia." IOP Conference Series: Earth and Environmental Science 1437, no. 1 (2024): 012007. https://doi.org/10.1088/1755-1315/1437/1/012007.

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Abstract Primary gold mineralization is associated with the hydrothermal processes. Interaction between the hydrothermal fluids and the wall rock resulting an alteration which characterized and indicated a mineralization process. The understanding of the mechanisms of alteration requires quantification of elemental changes in proximal to distal alteration zones. This study was conducted on an orogenic gold deposit at Awak Mas determine the lithogeochemical in each alteration zone caused by the hydrothermal processes. A total of eight schist rock samples geochemical data were applied in this st

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19

Whitbread, M. A., and C. L. Moore. "Two lithogeochemical approaches to the identification of alteration patterns at the Elura Zn–Pb–Ag deposit, Cobar, New South Wales, Australia: use of Pearce Element Ratio analysis and Isocon analysis." Geochemistry: Exploration, Environment, Analysis 4, no. 2 (2004): 129–41. http://dx.doi.org/10.1144/1467-7873/03-031.

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20

Li, Chuan, Zilong Li, Tao Wu, et al. "Metallogenic Characteristics and Formation Mechanism of Naomugeng Clay-Type Lithium Deposit in Central Inner Mongolia, China." Minerals 11, no. 3 (2021): 238. http://dx.doi.org/10.3390/min11030238.

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A newly discovered Naomugeng lithium mineralization area is located to the east of the Central Asian Orogenic Belt (CAOB). The lithium is hosted in the volcanic rocks of the Manketou’ebo Formation. The altered volcanic rocks mainly consist of quartz, orthoclase, chlorite, montmorillonite, calcite, and dolomite. Here, we present integrated studies of petrography, mineralogy, and geochemistry of the altered volcanic rocks (with an average Li2O content of 0.43 wt.%) collected from the drilling hole and trail trench to systematically investigate the occurrence of lithium, the mineralizing processe

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21

Kozak, P. "Meteors with multi-modal light curves: observations and qualitative models." Bulletin of Taras Shevchenko National University of Kyiv. Astronomy, no. 58 (2018): 48–55. http://dx.doi.org/10.17721/btsnua.2018.58.48-55.

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The problem of TV or video registration of meteors with anomalous light curves, in particular with multimodal and bimodal types is considered. The results of observations of two meteors from Perseid shower, obtained with the help of TV systems of super-isocon type are presented. The initial velocities of meteors were typical for Perseid shower meteors: 62.4 km/s and 58.4 km/s. One of the meteors has a light curve of a multimodal character, which can be explained by the fragmentation of the body. Another light curve has an evident bimodal type, which has no final explanation for the present. In

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22

Wagner, Thomas, and Nigel J. Cook. "Mineral reactions in sulphide systems as indicators of evolving fluid geochemistry – a case study from the Apollo mine, Siegerland, FRG." Mineralogical Magazine 61, no. 407 (1997): 573–90. http://dx.doi.org/10.1180/minmag.1997.061.407.09.

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AbstractThe textural and paragenetic relationships of sulphide and sulphosalt minerals within Cu-Pb-Sb-Bi hydrothermal vein mineralization at the Apollo mine, Siegerland, Germany, are interpreted in terms of various reaction sequences. An earlier primary sulphide mineralization hosted within a siderite vein of the Siegerland type, with pyrite, chalcopyrite, sphalerite and galena as main component phases, has been overprinted by Sb-, Bi- and Cu-rich fluids. This superposition resulted in the formation of new quartz-stibnite veins, and various mineral reactions with the primary sulphides includi

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23

Hertwig, A., W. V. Maresch, and H. P. Schertl. "Jadeitite and Related Rocks in Serpentinite Mélanges from the Rio San Juan Complex, Dominican Republic: Evidence for Both Isochemical Replacement and Metasomatic Desilication of Igneous Protoliths with Fluid-Assisted Jadeite Growth." Russian Geology and Geophysics 62, no. 5 (2021): 496–524. http://dx.doi.org/10.2113/rgg20204265.

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Abstract —This study presents an overview of the systematic petrography, mineralogy, and geochemistry of jadeitite and jadeite-rich rocks found as blocks in the serpentinite mélanges of the Rio San Juan Complex (RSJC) of the northern Dominican Republic. The RSJC is one of the remnants of the subduction/accretionary complex of the Great Caribbean Arc that once spanned the gap between North and South America, moved relatively eastward to its present position as the Lesser Antilles island arc, and left collisional fragments along the two continental margins. Our systematic collection of heterogen

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24

MA, MIAO, and XINHUI WANG. "Collection and taxonomic bias in herbarium specimens of Isodon (Lamiaceae)." Phytotaxa 687, no. 2 (2025): 127–75. https://doi.org/10.11646/phytotaxa.687.2.1.

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Isodon (Lamiaceae) is recognized as one of the largest and most taxonomically challenging genera worldwide. Nevertheless, research on the collection and taxonomic biases of Isodon remains limited. This study aimed to investigate the original materials’ status of Isodon, thus providing basic data for research on the systematics, biogeography, and conservation of the genus. Firstly, based on the iPlant database, the Catalogue of Life China, and the Catalogue of Life, the accepted species list of Isodon was obtained. Secondly, original materials of each species of Isodon were found by searching t

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25

Chen, Ya-Ping, Trevor C. Wilson, Ya-Dong Zhou, et al. "Isodon hsiwenii (Lamiaceae: Nepetoideae), A New Species From Yunnan, China." Systematic Botany 44, no. 4 (2019): 913–22. http://dx.doi.org/10.1600/036364419x15710776741486.

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Abstract—Isodon hsiwenii, a new species from Yunnan in Southwest China, is here described and illustrated. In order to clarify the phylogenetic placement of the new species within Isodon, Bayesian and maximum likelihood analyses based on two nuclear ribosomal DNA regions and four plastid DNA regions for 71 Asian Isodon species were conducted. The results indicate that I. hsiwenii is a member of the largest and poorly resolved Clade III, as sister species of I. hirtellus. Isodon hsiwenii can be distinguished from I. hirtellus by various morphological differences.

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Thomas, Alan, and P. Sunojkumar. "Lectotypification of the basionym of Isodon kurzii and Isodon nilgherricus." Phytotaxa 496, no. 1 (2021): 93–96. https://doi.org/10.11646/phytotaxa.496.1.6.

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Thomas, Alan, Sunojkumar, P. (2021): Lectotypification of the basionym of Isodon kurzii and Isodon nilgherricus. Phytotaxa 496 (1): 93-96, DOI: 10.11646/phytotaxa.496.1.6, URL: http://dx.doi.org/10.11646/phytotaxa.496.1.6

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27

Chen, Ya-Ping, Hua Peng, Alan J. Paton, and Chun-Lei Xiang. "Three new species of Isodon (Nepetoideae, Lamiaceae) from China." PhytoKeys 246 (September 19, 2024): 283–93. http://dx.doi.org/10.3897/phytokeys.246.130432.

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Three new species of Isodon (Lamiaceae) from China are described and illustrated, based on both morphological evidence and our recent phylogenomic studies of the genus. Isodon attenuatus, a herbaceous new species known only from the Fanjing Mountain, is shown to be sister to I. villosus, but they can be easily distinguished by leaf and inflorescence indumentum, calyx teeth shape and corolla tube morphology. Isodon gongshanensis, a herbaceous new species collected from the Hengduan Mountains in southwest China, represents a distinct lineage within the genus. Isodon sukungii, a shrubby new speci

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T. S., ALAN, KRISHNARAJ T. P., and SUNOJKUMAR P. "Nomenclatural notes on Isodon glaucocalyx and segregation from Isodon japonicus (Lamiaceae)." Phytotaxa 649, no. 2 (2024): 230–34. http://dx.doi.org/10.11646/phytotaxa.649.2.7.

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The Isodon genus comprises 100 species and is predominantly distributed in tropical and subtropical regions throughout Asia. The current study highlights the necessity of addressing the nomenclatural problem concerning Isodon japonicus and Isodon glaucocalyx. In 1832, Bentham treated Scutellaria japonica as the synonym of Plectranthus coetsa. Consequently, in some Indian botanical literature, P. coetsa is referred to as P. japonicus. Later, P. coetsa along with S. japonica was included as synonyms of P. glaucocalyx var. japonicus and due to publication priority resulting in I. glaucocalyx bein

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29

T., S. ALAN, P. KRISHNARAJ T., and SUNOJKUMAR P. "Nomenclatural notes on Isodon glaucocalyx and segregation from Isodon japonicus (Lamiaceae)." Phytotaxa 649, no. 2 (2024): 230–34. https://doi.org/10.11646/phytotaxa.649.2.7.

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T. S., ALAN, T. P., KRISHNARAJ, P., SUNOJKUMAR (2024): Nomenclatural notes on Isodon glaucocalyx and segregation from Isodon japonicus (Lamiaceae). Phytotaxa 649 (2): 230-234, DOI: 10.11646/phytotaxa.649.2.7, URL: http://dx.doi.org/10.11646/phytotaxa.649.2.7

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30

Chen, Ya-Ping, Hua Peng, Alan J. Paton, and Chun-Lei Xiang. "Three new species of Isodon (Nepetoideae, Lamiaceae) from China." PhytoKeys 246 (September 19, 2024): 283–93. https://doi.org/10.3897/phytokeys.246.130432.

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Three new species of <i>Isodon</i> (Lamiaceae) from China are described and illustrated, based on both morphological evidence and our recent phylogenomic studies of the genus. <i>Isodon attenuatus</i>, a herbaceous new species known only from the Fanjing Mountain, is shown to be sister to <i>I. villosus</i>, but they can be easily distinguished by leaf and inflorescence indumentum, calyx teeth shape and corolla tube morphology. <i>Isodon gongshanensis</i>, a herbaceous new species collected from the Hengduan Mountains in southwest China, represents a distinct lineage within the genus. <i>Isodo

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31

S., ALAN THOMAS, and P. SUNOJKUMAR. "Lectotypification of the basionym of Isodon kurzii and Isodon nilgherricus." Phytotaxa 496, no. 1 (2021): 93–96. http://dx.doi.org/10.11646/phytotaxa.496.1.6.

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Isodon (Schrad. ex Bentham 1832: 40) Spach (1840: 162), belonging to the family Lamiaceae, comprises about 100 species (Chen et al. 2016). Formerly, the species of this genus were included in the genus Plectranthus L’Héritier (1788: 84). In this article, we are designating the lectotype for Plectranthus kurzii Prain (1890: 296) and Plectranthus nilgherricus Bentham (1848: 57), basionyms of Isodon kurzii (Prain) Hara (1985: 234) and Isodon nilgherricus (Benth.) Hara (1985: 236), respectively. The lectotypification of Plectranthus nilgherricus is a second-step lectotypification as per Art. 9. 17

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32

Huang Hao, Chen Yiping, Zhang Hongjie, et al. "Diterpenoids from Isodon glutinosus." Phytochemistry 45, no. 3 (1997): 559–62. http://dx.doi.org/10.1016/s0031-9422(96)00808-4.

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Jia Wang, Zhong-Wen Lin, Qin-Shi Zhao, and Han-Dong Sun. "Diterpenoids from Isodon eriocalyx." Phytochemistry 47, no. 2 (1998): 307–9. http://dx.doi.org/10.1016/s0031-9422(97)00418-4.

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Zhao, Qin-Shi, Jun Tian, Jian-Min Yue, Shao-Nong Chen, Zhong-Wen Lin, and Han-Dong Sun. "Diterpenoids from isodon flavidus." Phytochemistry 48, no. 6 (1998): 1025–29. http://dx.doi.org/10.1016/s0031-9422(97)00608-0.

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Shao-Nong Chen, Hong-Jie Zhang, Zhong-Wen Lin, Yao-Zu Chen, and Han-Dong Sun. "Diterpenoids from Isodon gesneroides." Phytochemistry 48, no. 1 (1998): 155–58. http://dx.doi.org/10.1016/s0031-9422(97)00609-2.

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Zhao, Qin-Shi, Jun Tian, Jian-Min Yue, Shao-Nong Chen, Zhong-Wen Lin, and Han-Dong Sun. "diterpenoids from isodon melissoides." Phytochemistry 47, no. 6 (1998): 1089–92. http://dx.doi.org/10.1016/s0031-9422(98)80078-2.

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Na, Zhi, Wei Xiang, Xue-Mei Niu, et al. "Diterpenoids from Isodon enanderianus." Phytochemistry 60, no. 1 (2002): 55–60. http://dx.doi.org/10.1016/s0031-9422(02)00073-0.

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LI, Li-Mei, Jian-Xin PU, Wei-Lie XIAO, and Han-Dong SUN. "Triterpenes from Isodon xerophilus." Chinese Journal of Natural Medicines 10, no. 4 (2012): 307–10. http://dx.doi.org/10.1016/s1875-5364(12)60063-6.

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Wu, Shun-Hua, Hong-Jie Zang, Yi-Ping Chen, Zhong-Wen Lin, and Han-Dong Sun. "Diterpenoids from Isodon wikstroemioides." Phytochemistry 34, no. 4 (1993): 1099–102. http://dx.doi.org/10.1016/s0031-9422(00)90723-4.

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40

Jiang, Bei, Ze-Qin Lu, Hong-Jie Zhang, Qin-Shi Zhao, and Han-Dong Sun. "Diterpenoids from Isodon lophanthoides." Fitoterapia 71, no. 4 (2000): 360–64. http://dx.doi.org/10.1016/s0367-326x(00)00126-x.

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Zhang, Ji-Xia, Quan-Bin Han, Ai-Hua Zhao, and Han-Dong Sun. "Diterpenoids from Isodon japonica." Fitoterapia 74, no. 5 (2003): 435–38. http://dx.doi.org/10.1016/s0367-326x(03)00107-2.

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Zhao, Yong, Sheng-Xiong Huang, Wei-Lie Xiao, et al. "Diterpenoids from Isodon pharicus." Tetrahedron Letters 50, no. 17 (2009): 2019–23. http://dx.doi.org/10.1016/j.tetlet.2009.02.102.

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Ping, Zhang Rong, Zhang Hongjie, Lin Zhongwen, Zhen Yulin, and Sun Handong. "Diterpenoids from Isodon adenoloma." Phytochemistry 31, no. 12 (1992): 4237–40. http://dx.doi.org/10.1016/0031-9422(92)80450-s.

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Huang Hao, Sun Handong, and Zhao Shouxun. "Flavonoids from Isodon oresbius." Phytochemistry 42, no. 4 (1996): 1247–48. http://dx.doi.org/10.1016/0031-9422(96)00084-2.

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Hao, Huang, Sun Han-Dong, and Zhao Shou-Xun. "Triterpenoids of Isodon loxothyrsus." Phytochemistry 42, no. 6 (1996): 1665–66. http://dx.doi.org/10.1016/0031-9422(96)00204-x.

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Jiang, Hua-Yi, Wei-Guang Wang, Min Zhou, et al. "Diterpenoids from Isodon sculponeatus." Fitoterapia 93 (March 2014): 142–49. http://dx.doi.org/10.1016/j.fitote.2013.12.025.

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Jiang, Bei, Shuang-Xi Mei, Ai-Hua Zhao, Han-Dong Sun, Yang Lu, and Qi-Tai Zheng. "Diterpenoids from Isodon sculponeatus." Chinese Journal of Chemistry 20, no. 9 (2010): 887–90. http://dx.doi.org/10.1002/cjoc.20020200916.

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Jintao, Xue, Yu Shasha, Wang Jincai, Li Chunyan, Yang Mengya, and Shi Yongli. "Network Pharmacological Screening of the Active Ingredients and Hypoglycemic Effect of Isodon rubescens in the Treatment of Diabetes." Planta Medica 86, no. 08 (2020): 556–64. http://dx.doi.org/10.1055/a-1147-9196.

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AbstractThis study was firstly to study the relationship of “ingredient-target-pathway” and the pharmacological effects of Isodon rubescens for the treatment of diabetes. Based on a network pharmacology method, 138 active ingredients of Isodon rubescens were screened from the relative literatures, and their targets were confirmed by comparing these with the hypoglycemic targets in the DrugBank database. Results showed that Isodon rubescens contained 25 hypoglycemic ingredients, such as rabdoternin A, rabdoternin B, and epinodosinol. These ingredients could activate 6 hypoglycemic targets, incl

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Millard, Pierre, Baudoin Delépine, Matthieu Guionnet, Maud Heuillet, Floriant Bellvert, and Fabien Létisse. "IsoCor: isotope correction for high-resolution MS labeling experiments." Bioinformatics 35, no. 21 (2019): 4484–87. http://dx.doi.org/10.1093/bioinformatics/btz209.

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Abstract Summary Mass spectrometry (MS) is widely used for isotopic studies of metabolism and other (bio)chemical processes. Quantitative applications in systems and synthetic biology require to correct the raw MS data for the contribution of naturally occurring isotopes. Several tools are available to correct low-resolution MS data, and recent developments made substantial improvements by introducing resolution-dependent correction methods, hence opening the way to the correction of high-resolution MS (HRMS) data. Nevertheless, current HRMS correction methods partly fail to determine which is

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Li, Hsi-Wen. "Taxonomic Review of Isodon (Labiatae)." Journal of the Arnold Arboretum. 69, no. 4 (1988): 289–400. http://dx.doi.org/10.5962/p.324759.

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