E-viri
Recenzirano
-
Hower, James C.; Hoffman, Gretchen K.; Garrison, Trent M.
International journal of coal geology, 07/2013, Letnik: 114Journal Article
Inertinite macerals in the anthracite-rank Campanian Menefee Formation coal from the Cerrillos coalfield, Santa Fe County, New Mexico, show a range of forms consistent with forms found in lower-rank Mesozoic and younger coals. In particular, funginite is recognized in these anthracites, as is macrinite, and fusinite formed following microbial degradation. The macrinite in the Menefee coal has forms that are consistent with fungal and/or bacterial degradation of wood, followed by the ingestion of the latter material by insects or other animals, the regurgitation or excretion of the partially digested material, and the coprophagous recycling of the latter product. •Cretaceous New Mexico anthracite was studied.•Macrinite forms similar to other K and younger coals were observed.•Funginite was recognized among macerals.
![loading ... loading ...](themes/default/img/ajax-loading.gif)
Vnos na polico
Trajna povezava
- URL:
Faktor vpliva
Dostop do baze podatkov JCR je dovoljen samo uporabnikom iz Slovenije. Vaš trenutni IP-naslov ni na seznamu dovoljenih za dostop, zato je potrebna avtentikacija z ustreznim računom AAI.
Leto | Faktor vpliva | Izdaja | Kategorija | Razvrstitev | ||||
---|---|---|---|---|---|---|---|---|
JCR | SNIP | JCR | SNIP | JCR | SNIP | JCR | SNIP |
Baze podatkov, v katerih je revija indeksirana
Ime baze podatkov | Področje | Leto |
---|
Povezave do osebnih bibliografij avtorjev | Povezave do podatkov o raziskovalcih v sistemu SICRIS |
---|
Vir: Osebne bibliografije
in: SICRIS
To gradivo vam je dostopno v celotnem besedilu. Če kljub temu želite naročiti gradivo, kliknite gumb Nadaljuj.