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Zalaa Formation

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Journal Article

Lower Silurian conodonts from the Shine Jinst region, southwestern Mongolia Available to Purchase

Erika M. Danielsen, D. Jeffrey Over
Published: 01 January 2016
Journal of Paleontology (2016) 90 (1): 78–91.
DOI: https://doi.org/10.1017/jpa.2016.18
...Erika M. Danielsen; D. Jeffrey Over Abstract Lower Silurian conodonts were recovered from carbonate beds in the upper Zalaa and lower Sharchuluut formations at Yamaan Us in the Shine Jinst region, Gobi-Altai Zone, of southwestern Mongolia. Conodonts are described from the Zalaa Formation...
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(1) Geologic map of the Shine Jinst region showing the location of Yamaan Us, Pulkovo1942 datum updated to Monref97 GPS coordinates. (2) The Zalaa Formation overlain by the Sharchuluut Formation at Yamaan Us. Dashed line=formation contact, ‒ 0=0 m in Figure 2.

(1) Geologic map of the Shine Jinst region showing the location of Yamaan ... Available to Purchase

Published: 01 January 2016
Figure 1 (1) Geologic map of the Shine Jinst region showing the location of Yamaan Us, Pulkovo1942 datum updated to Monref97 GPS coordinates. (2) The Zalaa Formation overlain by the Sharchuluut Formation at Yamaan Us. Dashed line=formation contact, ‒ 0=0 m in Figure 2 .
Journal Article

INTERESTING PAPERS IN OTHER JOURNALS Available to Purchase

Journal: Economic Geology
Published: 01 September 2000
Economic Geology (2000) 95 (6): 1367–1370.
DOI: https://doi.org/10.2113/gsecongeo.95.6.1367
..., and Yu V. Shvarov 652 Tin-bearing borates of hulsite-paigeite series from skarn deposits of northeastern Russia: Composition and geochemical evidence for genesis— S.M. Aleksandrov, M.A. Troneva, and G.E. Kuril’chikova 676 Composition of mineral inclusions and formation of polycrystalline...
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Scanning electron microscope images of Llandovery conodonts from the upper Zalaa and lower Sharchuluut formations at Yamaan Us. Collection stored at the Research Center for Stratigraphy and Paleontology of the Mongolian University of Science and Technology, with call numbers CND/09-01–CND/09-28. Call numbers are followed by sample name: (1–7)Distomodus kentuckyensis; (1, 2) P1 elements, upper views (a), lower views (b); (1) CND/09-01, YU-Q; (2) CND/09-02, YU-Q; (3) P1 element, upper view, CND/09-03, YU-Q; (4) P2 element, posterior view (a), anterior view (b), CND/09-04, YU-G; (5) S0 element, posterior view (a), lateral view (b), CND/09-05, YU-G; (6) M element, outer lateral view, CND/09-06, YU-F; (7) M element, outer lateral view (a), oblique inner lateral view (b), outline indicating view in Fig. 3.7c, magnification of Fig. 3.7b to show striations (c), CND/09-07, YU-G. (8)Distomodus sp., S element, inner lateral view (a), outline indicating view in Fig. 3.8b, magnification of Fig. 3.8a to show striations (b), CND/09-08, YU-D. (9)Pseudooneotodus beckmanni, upper view (a), oblique lower view (b), CND/09-09, YU-I. (10)Panderodus serratus, lateral view, CND/09-10, YU-D. (11)Panderodus unicostatus, lateral view, CND/09-11, YU-N. (12, 13)Panderodus sp., lateral view; (12) CND/09-12, YU-D; (13) CND/09-13, YU-G. (14)Icriodella sp., P1 element, upper view (a), lower view (b), CND/09-14, YU-G. (15–18)Pseudolonchodina expansa; (15) S0 element, oblique lower view, CND/09-15, YU-G; (16) S0 element, posterior view, CND/09-16, YU-G; (17) P2 element, posterior view, CND/09-17, YU-D; (18) M element, inner lateral view, CND/09-18, YU-G. (19)Pseudolonchodina sp., S element, lateral view, CND/09-19, YU-D. (20–24)Pranognathus siluricus; (20) P2 element, outer lateral view (a), inner lateral view (b), CND/09-20, YU-G; (21) P2 element, upper view, CND/09-21, YU-G; (22) P1 element, lower view, CND/09-22, YU-G; (23, 24) P1 elements, lateral views (a), upper views (b); (23) CND/09-23, YU-G; (24) CND/09-24, YU-G. (25)Ozarkodina sp., P2/S element, lateral view, CND/09-25, YU-D. (26–28)Ozarkodina hassi; (26, 27) P2 elements, lateral views; (26) CND/09-26, YU-Q; (27) CND/09-27, YU-G; (28) P1 element, lateral view (a), upper view (b), CND/09-28, YU-D. Scale bars=100 µm.

Scanning electron microscope images of Llandovery conodonts from the upper ... Available to Purchase

Published: 01 January 2016
Figure 3 Scanning electron microscope images of Llandovery conodonts from the upper Zalaa and lower Sharchuluut formations at Yamaan Us. Collection stored at the Research Center for Stratigraphy and Paleontology of the Mongolian University of Science and Technology, with call numbers CND/09-01