1-7 OF 7 RESULTS FOR

Songkarsu Formation

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Journal: GSA Bulletin
Published: 01 May 2013
GSA Bulletin (2013) 125 (5-6): 932–944.
... and Songkarsu Formations of terrestrial molasse in the southeastern part of the Kalamaili belt, shed from the rising Kalamaili orogen, record the orogenic history. The strata consist of proximal conglomerate thinning to distal fine-grained sandstone and mudstone. Poorly sorted conglomerate is composed...
FIGURES | View All (8)
Image
(A) Kalamaili mélange containing components of ophiolites mixed in strongly...
Published: 01 May 2013
sandstone and conglomerate of Tamugang Formation in the Shuangjingzi area. (D) Conglomerate intercalated with thin-bedded sandstone of the Songkarsu Formation in the Shuangjingzi area. (E) Imbricated gravels in conglomerate of the Songkarsu Formation. (F) Conglomerate of the Songkarsu Formation containing
Image
Frequency histograms for U-Pb ages of detrital zircons from the Tamugang Fo...
Published: 01 May 2013
Figure 5. Frequency histograms for U-Pb ages of detrital zircons from the Tamugang Formation (A) (sample K-13) and the Songkarsu Formation (B) (sample K-24) and isoplot outputs for the youngest detrital grain within Tamugang Formation (C) and Songkarsu Formation (D). Vertical lines in C and D
Image
Typical molasse in the Kalamaili orogenic belt. (A) Depositional model of m...
Published: 01 May 2013
) and that of the Dishuiquan area is from BGMRXUAR (1996) and Wang et al. (2010) . (C) Lithological distributions of gravel clasts in conglomerate of the Songkarsu Formation. (D) Rose diagrams of imbricated clasts in the Songkarsu Formation. Arrows are the vector-mean–restored paleocurrent directions calculated
Image
The distribution of U-Pb ages of detrital zircons from the Kalamaili, Tamug...
Published: 01 May 2013
Figure 7. The distribution of U-Pb ages of detrital zircons from the Kalamaili, Tamugang, and Songkarsu Formations.
Image
SENSITIVE HIGH-RESOLUTION ION MICROPROBE (SHRIMP) U-Pb DATA OF ZIRCONS OF T...
Published: 01 May 2013
TABLE 1. SENSITIVE HIGH-RESOLUTION ION MICROPROBE (SHRIMP) U-Pb DATA OF ZIRCONS OF TWO GRANITIC COBBLES (SAMPLE SHJ-18-1 AND SHJ-19-3) FROM THE SONGKARSU FORMATION AND ONE TRACHYANDENSITE SAMPLE (SHJ-8-4) FROM THE BATAMAYINEISHAN FORMATION
Image
U-Pb concordia diagrams of zircons from K-feldspar granite cobble (A) (samp...
Published: 01 May 2013
Figure 6. U-Pb concordia diagrams of zircons from K-feldspar granite cobble (A) (sample SHJ-18–1) and biotite granite cobble (B) (sample SHJ-19–3) in the Songkarsu Formation and trachyandsite in the Batamayineishan Formation (C) (sample SHJ-8–4). MSWD—mean square of weighted deviates.