The comparative studies on micromorphological features in diagnostic horizons of Stagnic Anthrosols, Ustic Ferrosols and Ustic Vertosols in southwestern China were conducted to underpin the rationale for Chinese Soil ...The comparative studies on micromorphological features in diagnostic horizons of Stagnic Anthrosols, Ustic Ferrosols and Ustic Vertosols in southwestern China were conducted to underpin the rationale for Chinese Soil Taxonomy. The following findings were explored: (1) Stagnic Anthrosols had the specific micromorphological features, e.g., the humic formation in anthrostagnic epipedon, the platy structures in plow subhorizon, the secondary formation of ferromanganese and the weakly optical-orientation clay domains in hydragric horizon, etc.: (2) The groundmasses of ferric horizon in Ustic Ferrosols appeared in hue of 2.5YR or redder, and had pellicular grain structure; (3) Ustic Vertosols had a crust horizon (Acr), and crack structure dominated in Acr and angular blocky structure in disturbed horizon; (4) Because of the distinct differences in micromorphological features among these three soils, the specific micromorphological features might be employed as diagnostic horizons to differentiate soils while the quantifiable micromorphological features might potentially be selected as diagnostic indices for Chinese soil taxonomic classification.展开更多
OBJECTIVE To investigate the detection of sentinel lymphnode (SLN) micrometastasis (MM) and the clinical significancein patients with Dukes-B colorectal carcinoma (CRC) using H&Estained slides.METHODS In a prospec...OBJECTIVE To investigate the detection of sentinel lymphnode (SLN) micrometastasis (MM) and the clinical significancein patients with Dukes-B colorectal carcinoma (CRC) using H&Estained slides.METHODS In a prospective study of 64 patients with Dukes-BCRC undergoing radical surgery,routine H&E staining combinedwith the immunohistochemical SP method was used to detect theexpression of the cytokeratin 20 (CK20) and telomerase (TLMA)in 122 SLNs from 61 of the 64 cases.During a 3-year follow up,the patients'clinicopathologic parameters data,survival and theirrelationship were collected and analyzed.RESULTS i) In 6 out of the 61 cases with successful mapping,9SLNs were positive after routine detection using H&E staining.ii) In the other 55 with negative results from H&E staining,thepositive rate of CK20 expression was 27.3% (15/55),and thepositive rate of TLMA 21.8% (12/55),after immunohistochemicalexamination (IHC) on the SLN.iii) Detection by combining the 2methods showed that the micrometastasis rate was 38.2% (21/55).iv) The recurrence or metastasis rate of CRC was significantlyhigher in the Dukes-B patients with sentinel lymph nodemicrometastasis (SLNMM) (+) than in those with SLNMM (-)(P<0.05),and simultaneously,the survival rate decreased by alarge margin in the patients with SLNMM (+),compared to thosewith SLNMM (-) (P<0.05).There were significant differences inthe recurrence or metastasis rate of cancer and the survival ratebetween the Dukes-B patients with SLNMM (-) and the Dukes-Cpatients (P<0.05).CONCLUSION Examination of anti-CK20 and anti-TLMA usingimmunohistochemical staining can be used to detect SLNMM,andthe combined examination of the 2 can increase the detection rate.The detection of SLNMM can precisely determine the Dukes stageof colorectal carcinoma,which is of help in directing postoperativeadjunctive therapy and in assessing prognosis.展开更多
Through analysis of geological characteristics of the gold deposit,the shape,occurrence,and spatial distribution of ore-controlling fault plane in the Shanhou mining area were investigated,and the regularities of enri...Through analysis of geological characteristics of the gold deposit,the shape,occurrence,and spatial distribution of ore-controlling fault plane in the Shanhou mining area were investigated,and the regularities of enrichment and emplacement of ore body were summarized. The analysis shows that the Shanhou gold deposit was controlled by NE-NNE Zhaoping fault zone; the fault gouge developed in fault zone provides a barrier to ore-bearing hydrothermal solution,and the industrial ore body is all distributed within 40 m of footwall of main fault plane. The industrial ore body is mainly enriched in the NE positions of fault where the deep dips changed to flat dips,and shows the obvious regularity of NE lateral trending with angle around 75°. The stress analysis of fault in mineralization epoch showed that the ore-controlling structure presented the characteristics of righthanded rotation inverse-fault activity in mineralization epoch,and the host space tended to occur in NE regional tension positions where the dips become flat in the strike of fault,causing emplacement of ore body. It is thought by combining equal interval distribution of deposit with spatial variation of industrial ore body and orecontrolling fault structure that the Shanhou gold deposit recurred in regularity and the non-ore interval occurred in the ore body. Meanwhile,it is predicted that the favorable target area of prospecting lies in the areas of deep main fault plane with NE strike( > 30°) and the deep dips changing to flat dips in the Shanhou mining area,and the prospecting should be emphasized. The favorable deep mineralization prospect exists in middle Beibo mining area,where is the key area for future prospecting.展开更多
LA-ICP-MS zircon U-Pb isotopic dating and rock geochemical analysis were done of the Xarru granite in the middle section of the Yarlung Zangbo junction zone. Zircon 2-6pb/Z38u weighted mean ages of 474.9±2.3 and ...LA-ICP-MS zircon U-Pb isotopic dating and rock geochemical analysis were done of the Xarru granite in the middle section of the Yarlung Zangbo junction zone. Zircon 2-6pb/Z38u weighted mean ages of 474.9±2.3 and 478.3±1.7 Ma have been obtained for two gneiss granite samples respectively, which represent the formation age of the granite. This is the first discovery of the Early Ordovician magmatism in the Yarlung Zangbo junction zone. The rocks are high-K calcic-alkalic granite, contain tour- maline but not hornblende, with aluminum saturation index （ASI） of A/CNK〉I.1 （1.10-1.20）, and are enriched in Rb, Th and U and relatively depleted in Ba, Nb, Sr, Zr, Ti and Eu. They are strongly peraluminous S-type granite, resulting from partial melting of argillaceous components in the crust in a syn-collisional setting. According to previous studies as well as the analy- sis in this paper, the formation of the Xarru granite is probably related to the Andean-type orogeny in the process of subduction of the Proto-Tethys Ocean towards the Gondwanaland, and it is a product of partial melting of the thickened upper crust as a result of collision between blocks or micro-blocks in the northern margin of the Gondwana supercontinent in the process of oceanic subduction. The Xarru granite is identified as the Early Ordovician granite, indicating that the wall rocks had probably formed in the Cambrian or Precambrian.展开更多
基金supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (Grant No. KZCX2-YW-409)
文摘The comparative studies on micromorphological features in diagnostic horizons of Stagnic Anthrosols, Ustic Ferrosols and Ustic Vertosols in southwestern China were conducted to underpin the rationale for Chinese Soil Taxonomy. The following findings were explored: (1) Stagnic Anthrosols had the specific micromorphological features, e.g., the humic formation in anthrostagnic epipedon, the platy structures in plow subhorizon, the secondary formation of ferromanganese and the weakly optical-orientation clay domains in hydragric horizon, etc.: (2) The groundmasses of ferric horizon in Ustic Ferrosols appeared in hue of 2.5YR or redder, and had pellicular grain structure; (3) Ustic Vertosols had a crust horizon (Acr), and crack structure dominated in Acr and angular blocky structure in disturbed horizon; (4) Because of the distinct differences in micromorphological features among these three soils, the specific micromorphological features might be employed as diagnostic horizons to differentiate soils while the quantifiable micromorphological features might potentially be selected as diagnostic indices for Chinese soil taxonomic classification.
基金supported by a grant from Gansu Provincial Program for Tackling Key Problems in Science and Technology,China (No.2GS064-B43-020-36)
文摘OBJECTIVE To investigate the detection of sentinel lymphnode (SLN) micrometastasis (MM) and the clinical significancein patients with Dukes-B colorectal carcinoma (CRC) using H&Estained slides.METHODS In a prospective study of 64 patients with Dukes-BCRC undergoing radical surgery,routine H&E staining combinedwith the immunohistochemical SP method was used to detect theexpression of the cytokeratin 20 (CK20) and telomerase (TLMA)in 122 SLNs from 61 of the 64 cases.During a 3-year follow up,the patients'clinicopathologic parameters data,survival and theirrelationship were collected and analyzed.RESULTS i) In 6 out of the 61 cases with successful mapping,9SLNs were positive after routine detection using H&E staining.ii) In the other 55 with negative results from H&E staining,thepositive rate of CK20 expression was 27.3% (15/55),and thepositive rate of TLMA 21.8% (12/55),after immunohistochemicalexamination (IHC) on the SLN.iii) Detection by combining the 2methods showed that the micrometastasis rate was 38.2% (21/55).iv) The recurrence or metastasis rate of CRC was significantlyhigher in the Dukes-B patients with sentinel lymph nodemicrometastasis (SLNMM) (+) than in those with SLNMM (-)(P<0.05),and simultaneously,the survival rate decreased by alarge margin in the patients with SLNMM (+),compared to thosewith SLNMM (-) (P<0.05).There were significant differences inthe recurrence or metastasis rate of cancer and the survival ratebetween the Dukes-B patients with SLNMM (-) and the Dukes-Cpatients (P<0.05).CONCLUSION Examination of anti-CK20 and anti-TLMA usingimmunohistochemical staining can be used to detect SLNMM,andthe combined examination of the 2 can increase the detection rate.The detection of SLNMM can precisely determine the Dukes stageof colorectal carcinoma,which is of help in directing postoperativeadjunctive therapy and in assessing prognosis.
基金Project of Shanhou Gold Deposit of Laixi of Shandong Province(SDLX2012-3-28)
文摘Through analysis of geological characteristics of the gold deposit,the shape,occurrence,and spatial distribution of ore-controlling fault plane in the Shanhou mining area were investigated,and the regularities of enrichment and emplacement of ore body were summarized. The analysis shows that the Shanhou gold deposit was controlled by NE-NNE Zhaoping fault zone; the fault gouge developed in fault zone provides a barrier to ore-bearing hydrothermal solution,and the industrial ore body is all distributed within 40 m of footwall of main fault plane. The industrial ore body is mainly enriched in the NE positions of fault where the deep dips changed to flat dips,and shows the obvious regularity of NE lateral trending with angle around 75°. The stress analysis of fault in mineralization epoch showed that the ore-controlling structure presented the characteristics of righthanded rotation inverse-fault activity in mineralization epoch,and the host space tended to occur in NE regional tension positions where the dips become flat in the strike of fault,causing emplacement of ore body. It is thought by combining equal interval distribution of deposit with spatial variation of industrial ore body and orecontrolling fault structure that the Shanhou gold deposit recurred in regularity and the non-ore interval occurred in the ore body. Meanwhile,it is predicted that the favorable target area of prospecting lies in the areas of deep main fault plane with NE strike( > 30°) and the deep dips changing to flat dips in the Shanhou mining area,and the prospecting should be emphasized. The favorable deep mineralization prospect exists in middle Beibo mining area,where is the key area for future prospecting.
基金supported by China Geologi-cal Survey Project(Grant No.1212011086039)
文摘LA-ICP-MS zircon U-Pb isotopic dating and rock geochemical analysis were done of the Xarru granite in the middle section of the Yarlung Zangbo junction zone. Zircon 2-6pb/Z38u weighted mean ages of 474.9±2.3 and 478.3±1.7 Ma have been obtained for two gneiss granite samples respectively, which represent the formation age of the granite. This is the first discovery of the Early Ordovician magmatism in the Yarlung Zangbo junction zone. The rocks are high-K calcic-alkalic granite, contain tour- maline but not hornblende, with aluminum saturation index （ASI） of A/CNK〉I.1 （1.10-1.20）, and are enriched in Rb, Th and U and relatively depleted in Ba, Nb, Sr, Zr, Ti and Eu. They are strongly peraluminous S-type granite, resulting from partial melting of argillaceous components in the crust in a syn-collisional setting. According to previous studies as well as the analy- sis in this paper, the formation of the Xarru granite is probably related to the Andean-type orogeny in the process of subduction of the Proto-Tethys Ocean towards the Gondwanaland, and it is a product of partial melting of the thickened upper crust as a result of collision between blocks or micro-blocks in the northern margin of the Gondwana supercontinent in the process of oceanic subduction. The Xarru granite is identified as the Early Ordovician granite, indicating that the wall rocks had probably formed in the Cambrian or Precambrian.
