Clay Minerals

journal
Place periodical Q4779306
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Clay Minerals

Summary

Clay Minerals is a periodical[1].

Key Facts

  • Clay Minerals's instance of is recorded as periodical[2].
  • Clay Minerals's editor is recorded as Enver Murad[3].
  • Clay Minerals's publisher is recorded as Cambridge University Press[4].
  • Clay Minerals's ISSN is recorded as 0009-8558[5].
  • Clay Minerals's ISSN is recorded as 1471-8030[6].
  • Clay Minerals's language of work or name is recorded as English[7].
  • Clay Minerals's archives at is recorded as Portico[8].
  • Clay Minerals's archives at is recorded as CLOCKSS[9].
  • Clay Minerals's country of origin is recorded as United Kingdom[10].
  • Clay Minerals's official website is recorded as http://claymin.geoscienceworld.org/[11].
  • Clay Minerals's official website is recorded as http://www.ingentaconnect.com/content/minsoc/cm[12].
  • Clay Minerals's official website is recorded as https://www.cambridge.org/core/journals/clay-minerals[13].
  • Clay Minerals's NLM Unique ID is recorded as 100971321[14].
  • Clay Minerals's ERA Journal ID is recorded as 34464[15].
  • Clay Minerals's Scopus source ID is recorded as 22523[16].
  • Clay Minerals's Danish Bibliometric Research Indicator level is recorded as 1[17].
  • Clay Minerals's Danish Bibliometric Research Indicator is recorded as 15799[18].
  • Clay Minerals's JUFO ID is recorded as 53521[19].
  • Clay Minerals's bibcode is recorded as ClMin[20].
  • Clay Minerals's title is recorded as Clay Minerals[21].
  • Clay Minerals's Google Knowledge Graph ID is recorded as /g/11_pkrx40[22].
  • Clay Minerals's OpenCitations bibliographic resource ID is recorded as 646420[23].
  • Clay Minerals's ISSN-L is recorded as 0009-8558[24].
  • Clay Minerals's Scilit journal ID is recorded as 584732[25].
  • Clay Minerals's Crossref journal ID is recorded as 5841[26].

Body

Designation and Status

Clay Minerals's instance of is recorded as periodical[2].

References

Programmatic citations — every numbered marker resolves to a verifiable graph row below.

Direct Wikidata claims

  1. [2] ↑ . wikidata.org.
  2. [3] ↑ . degruyter.com. Retrieved . degruyter.com. Provenance: wikidata.org.
  3. [4] ↑ . cambridge.org. Retrieved . cambridge.org. Provenance: wikidata.org.
  4. [5] ↑ . wikidata.org.
  5. [6] ↑ . ERA 2012 journal list. wikidata.org.
  6. [7] ↑ . ISSN Portal. wikidata.org.
  7. [8] ↑ . wikidata.org.
  8. [9] ↑ . wikidata.org.
  9. [10] ↑ . ISSN Portal. wikidata.org.
  10. [11] ↑ . wikidata.org.
  11. [12] ↑ . ISSN Portal. wikidata.org.
  12. [13] ↑ . ISSN Portal. wikidata.org.
  13. [14] ↑ . wikidata.org.
  14. [15] ↑ . ERA 2010 journal list. wikidata.org.
  15. [16] ↑ . Scopus. wikidata.org.
  16. [17] ↑ . BFI 2012 journal list. wikidata.org.
  17. [18] ↑ . BFI 2012 journal list. wikidata.org.
  18. [19] ↑ . wikidata.org.
  19. [20] ↑ . wikidata.org.
  20. [21] ↑ . ISSN Portal. wikidata.org.
  21. [22] ↑ . wikidata.org.
  22. [23] ↑ . OpenCitations Corpus. wikidata.org.
  23. [24] ↑ . wikidata.org.
  24. [25] ↑ . wikidata.org.
  25. [26] ↑ . wikidata.org.

Class ancestry

  1. [1] ↑ . Wikidata. wikidata.org.

📑 Cite this page

Use these citations when quoting this entity in research, articles, AI prompts, or wherever provenance matters. We aggregate Wikidata + Wikipedia + authoritative open-data sources; the stitched, scored, cross-referenced view is what 4ort.xyz contributes.

APA 4ort.xyz Knowledge Graph. (2026). Clay Minerals. Retrieved May 3, 2026, from https://4ort.xyz/entity/clay-minerals-q4779306
MLA “Clay Minerals.” 4ort.xyz Knowledge Graph, 4ort.xyz, 3 May. 2026, https://4ort.xyz/entity/clay-minerals-q4779306.
BibTeX @misc{4ortxyz_clay-minerals-q4779306_2026, author = {{4ort.xyz Knowledge Graph}}, title = {{Clay Minerals}}, year = {2026}, url = {https://4ort.xyz/entity/clay-minerals-q4779306}, note = {Accessed: 2026-05-03}}
LLM prompt According to 4ort.xyz Knowledge Graph (aggregator of Wikidata, Wikipedia, and authoritative open-data sources): Clay Minerals — https://4ort.xyz/entity/clay-minerals-q4779306 (retrieved 2026-05-03)

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