scholarly journals Supplemental Material: Age, material source, and formation mechanism of bedding-parallel calcite beef veins: Case from the mature Eocene lacustrineshales in the Biyang Sag, Nanxiang Basin, China

2021 ◽  
Author(s):  
Ao Su ◽  
et al.

Figure S1: Correlations of vein density vs. TOC, calcite, and dolomite contents of host shales; Figure S2: The box plots of calcite contents in shale samples with and without beef veins; Table S1: LA-MC-ICP-MS carbonate U-Pb dating data.

2021 ◽  
Author(s):  
Ao Su ◽  
et al.

Figure S1: Correlations of vein density vs. TOC, calcite, and dolomite contents of host shales; Figure S2: The box plots of calcite contents in shale samples with and without beef veins; Table S1: LA-MC-ICP-MS carbonate U-Pb dating data.


2021 ◽  
pp. 1-41
Author(s):  
Lianfu Hai ◽  
Qinghai Xu ◽  
Caixia Mu ◽  
Rui Tao ◽  
Lei Wang ◽  
...  

In the Tanshan area, which is at the Liupanshui Basin, abundant oil shale resources are associated with coals. We analyzed the cores, geochemistry of rare earth elements (REE) and trace element of oil shale with ICP-MS technology to define the palaeo-sedimentary environment, material source and geological significance of oil shale in this area. The results of the summed compositions of REE, and the total REE contents (SREE), in the Yan'an Formation oil shale are slightly higher than the global average of the composition of the upper continental crustal (UCC) and are lower than that of North American shales. The REE distribution pattern is characterized by right-inclined enrichment of light rare earth elements (LREE) and relative loss of heavy rare earth elements (HREE), which reflects the characteristics of crustal source deposition. There is a moderate degree of differentiation among LREE, while the differences among HREE are not obvious. The dEu values show a weak negative anomaly and the dCe values show no anomaly, which are generally consistent with the distribution of REE in the upper crust. The characteristics of REE and trace elements indicate that the oil shale formed in an oxygen-poor reducing environment and that the paleoclimatic conditions were relatively warm and humid. The degree of differentiation of REE indicates that the sedimentation rate in the study area was low, which reflected the characteristics of relatively deep sedimentary water bodies and distant source areas. The results also proved that the source rock mainly consisted of calcareous mudstone, and a small amount of granite was also mixed in.


2021 ◽  
Author(s):  
Qing Zheng ◽  
Yaru Hu ◽  
Ayuan Xiong ◽  
Ying Su ◽  
Zihao Wang ◽  
...  

Elucidating the organometallic interactions in Baijiu will promote a deeper understanding of the flavour formation mechanism during Baijiu aging. However, the organometallic interactions during aging is difficult to explore because...


2017 ◽  
Vol 8 (2) ◽  
Author(s):  
Ronaldo Irzon

Abstract Kulon Progo is located in the southern part of Yogyakarta Special Province, Indonesia. The regency is famous of some tourist beach points. This study discusses the compositiom of beach sand samples in three coastal areas in Kulon Progo: Karangwuni, Glagah, and Congot in relation to environmental issues. Seven samples of four locations were megascopically descripted and analyzed using XRF and ICP-MS for geochemistry contents. Four of samples are beach sands from the surface whilst the others were collected from about 50 cm below surface. Box plots show maximum Cr outlier and minimum most of REE outliers in the group of beach sand samples. Nickel and chrome tenor anomalies were detected in samples from coastline of Karangwuni and Glagah. On the other hand, no Ni and Cr anamalies were indentified in the two samples 200 m from the seashore of Karangwuni nor the two samples near Congot seashore. In the polluted location, the two heavy metals are relatively concentrated in the surface. Two volcanic rock samples from the Andesite domain are selected to trace the origin of the heavy metals. The wastes of basic metal mining in northern Kulon Progo together with urban activities and several industries in Wates were then transported through the Serang River to Indian Ocean. Tidal currents helps the heavy metals to be deposited in the coastal areas near the mouth of Serang River. This study also concluded that folk gold mining activity in Sangon is not the source of Ni and Cr pollution to the coast of Kulon Progo.Keyword: geochemistry, beach sand, Kulon Progo, heavy metals pollution. Sari Kulon Progo berlokasi di bagian selatan Provinsi Daerah Istimewa Jakarta, Indonesia. Kabupaten ini terkenal dengan beberapa lokasi wisata pantai. Studi ini membahas mengenai komposisi pasir pantai pada tiga lokasi pantai di Kulon Progo: Karangwuni, Glagah, dan Congot terkait dengan masalah lingkungan. Tujuh contoh dari empat lokasi penelitian telah dideskripsikan secara megaskopis dan dianalisis kandungan geokimianya menggunakan XRF dan ICP-MS. Empat contoh merupakan pasir pantai yang berasal dari permukaan sedangkan contoh lain berasal dari 50 cm di bawah permukaan. Box plot dengan jelas menunjukkan keberadaan maximum outlier pada Cr dan minimum ourlier pada banyak elemen dari REE pada kelompok contoh pasir pantai. Anomali tinggi nikel dan krom terdeteksi pada seluruh contoh yang berada dekat tepi pantai di Karangwuni dan Glagah. Namun demikian, tidak terdapat anomali Ni dan Cr pada dua contoh yang berasal dari 200 m sebelum tepi pantai Karangwuni maupun dua contoh dari Pantai Congot. Pada titik yang tercemar polusi, dua logam berat ini lebih terkonsentrasi pada bagian permukaan. Dua batuan vulkanik dari wilayah Andesit dipilih dalam menelusuri asal muasal logam berat tersebut. Sampah sisa penambangan logam dasar bersama dengan aktifitas perkotaan dan industri di Kulon Progo telah terbawa oleh aliran Sungai Serang menuju Samudera Hindia. Arus bolak-balik air laut membantu logam berat tersebut terdepositkan di wilayah pantai dekat dengan mulut Sungai Serang. Studi ini turut menyimpulkan bahwa penambangan emas rakyat di Sangon bukan sebagai sumber pencemaran Ni dan Cr di tepi pantai Kulon ProgoKata kunci: geokimia, pasir pantai, Kulon Progo, polusi logam berat


2013 ◽  
Vol 405-408 ◽  
pp. 602-606
Author(s):  
Tian Fan Dai

the paper introduces the basic characteristics of the landslide, analyzes the formation mechanism of the landslide, I think that the thick and loose efflorescent colluvial deposit on landslide offer material source of the landslide; Steep hill provides effective free surface for the landslide ; Heavy rainfall and human engineering activities are the main factors for the stability of the landslide. According to rock physical mechanics test and stability calculation results under different working conditions, afford a stability evaluation for the landslide. The results show that the landslide may lose stability when cutting slope in the leading edge, loading in trailing edge and suffering heavy rainfall, we should take the necessary measures to prevent and control.


Planta Medica ◽  
2015 ◽  
Vol 81 (16) ◽  
Author(s):  
Y Kho ◽  
M Kim ◽  
NY Park ◽  
H Park ◽  
JH Shin

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