CĂRȚI ÎN ENGLEZĂ ÎN LEGĂTURĂ CU «ECHINODERMAL»
Descoperă întrebuințarea
echinodermal în următoarea selecție bibliografică. Cărți în legătură cu
echinodermal și extrase din aceasta pentru a furniza contextul de întrebuințare al acestuia în literatura Engleză.
1
Transactions of the Royal Society of South Australia
Fine yellow sands (polyzoal and echinodermal debris at 820—835). 880 — 928.
Fine yellow calciferous sands (polyzoal and echinodermal debris at 905 — 910).
928 — 931. Yellow sandy clay with fragments of Eupatagus sp. 931 — 970.
Royal Society of South Australia, Walter Howchin,
1896
2
Transactions of the Royal Society of South Australia
Calcareous silt, with much polyzoal debris, chiefly Cellepone at 778 feet. 810 —
880. Fine yellow sands (polyzoal and echinodermal debris at 820—835). 880 —
928. Fine yellow calciferous sands (polyzoal and echinodermal debris at 905 ...
Fine yellow sands (polyzoal and echinodermal debris at 820—835). 880 — 928.
Fine yellow calciferous sands (polyzoal and echinodermal debris at 905 — 910).
928 — 931. Yellow sandy clay with fragments of Eupatagus sp. 931 — 970.
Royal Society of South Australia,
1896
4
Transactions and Proceedings and Report of the Royal Society ...
Fine yellow sands (polyzoal and echinodermal debris at 820—835). 880 — 928.
Fine yellow calciferous sands (polyzoal and echinodermal debris at 905 — 910).
928 — 931. Yellow sandy clay with fragments of Eupatagus sp. 931 — 970.
Royal Society of South Australia,
1898
Model (a) refers to the growth of “tooth” (zahn) cement, whereas model (b)
applies to the growth of facet cement on stereom echinodermal calcite. (Modified
from Neugebauer, I979.) Elemental geochemistry The rapid destruction,
occlusion by ...
G.V. Chilingarian, K.H. Wolf,
1994
6
Evaporites Through Space and Time
These biounits are: (1) an echinodermal-gastropodal unit; (2) a miliolidal unit;
and (3) an echinodermal unit (Fig. 16). However, the echinodermal and miliolidal
units were recorded in the Jeribe Formation of traverse B-B' (Fig. 17). The lateral
...
B. Charlotte Schreiber, S. Lugli, M. Ba̜bel,
2007
7
Echinoderm faunas from the bromide formation (middle ...
Limestone, tan to greenish-gray, medium-grained, medium-bedded, well-
indurated, fossiliferous, echinodermal, eroding into ledge 0.18 6. Shale, tan to
red-brown, thin-bedded, weakly indurated, echinodermal 0.15 7. Limestone, gray
to tan, ...
8
Guidebook: Geology of the Arbuckle Mountains along ...
33* Limestone, bluish-gray, coarse-grained, massive, we ll -indurated, fossilifer-
ous, echinodermal; eroding into a ledge 1.0 3^. Shale, bluish-gray, platy, weakly -
indurated, with many 1- to l*-inch beds of fine-grained argillaceous nodular ...
Robert O Fay, Ardmore Geological Society,
1969
related to the continuity of the larval CA nervous system. Further investigations
are needed to show how continuous axon tracts are formed during the ontogeny
of echinodermal larvae. In the starfish larvae of A. typicus, early bi- pinaria do not
...
10
Notes on the Mesozoic and Tertiary stratigraphy in the Velez ...
2. packed pelmicrosparites containing minor amounts of silt-sized quartz, with
Globochaete alpina LOMBARD, Radiolaria and echinodermal fragments. The
matrix is a packed echinodermal biomicrite. The brecciaceous limestone is
composed ...