From the pyramids of Giza to the tombs of Thebes at Luxor, the glorious ancient Egyptian history has produced remarkable architecture. Sadly, tourists, numbering nearly four million per year, have taken a heavy toll o...From the pyramids of Giza to the tombs of Thebes at Luxor, the glorious ancient Egyptian history has produced remarkable architecture. Sadly, tourists, numbering nearly four million per year, have taken a heavy toll on many of these ancient structures. Of particular concern are many of tombs located opposite Luxor on the western bank of the Nile. Digital reconstruction of these tombs has the potential of helping to document and preserve these important historical structures. Issues concernng new and unique problems involving the photographing and digital reconstruction of these tombs are addressed. Techniques for removing image distortions, recovering 3-D shapes and correcting for lighting imbalances are discussed. A complete reconstruction of the tomb of Sennediem is shown.展开更多
Abstract: This paper discusses the distribution pattern and geological significance of the carbon and oxygen isotopes (δ13C and δ18O) in the depositional sequences of Gaoyuzhuangian, Yangzhuangian and Wumishanian ag...Abstract: This paper discusses the distribution pattern and geological significance of the carbon and oxygen isotopes (δ13C and δ18O) in the depositional sequences of Gaoyuzhuangian, Yangzhuangian and Wumishanian ages of the established Middle and Upper Proterozoic sequence stratigraphic framework in the Ming Tombs area lying in western Yanshan Mountain of Beijing. Besides, sketchy determination of δ13C and δ18O was also performed for other formations and members. The analytical results show the following: under the condition of clear-water carbonate sediments, δ13C and δ18O, featuring smaller variation of δ13C but larger variation of δ18O, can well delineate the relative change of sea level, which reflects the difference of primary sedimentary settings; in the presence of terrigenous substances, δ13C values vary greatly while δ18O slightly; the carbon and oxygen isotopes show marked changes at sequence boundaries. Besides, particular patterns can be found in regard to the distribution of carbon and oxygen isotopes within the sequences.展开更多
Built between 1368 and 1911, The Imperial Tombs of the Ming （1368- 1644） and Qing （1644-1911） dynaslies includes Xianling Tombs of theMing Dynast）. Eastern and Western Qing Tornbs, Xiaoling Tomb of the Ming Dynasty.
文摘From the pyramids of Giza to the tombs of Thebes at Luxor, the glorious ancient Egyptian history has produced remarkable architecture. Sadly, tourists, numbering nearly four million per year, have taken a heavy toll on many of these ancient structures. Of particular concern are many of tombs located opposite Luxor on the western bank of the Nile. Digital reconstruction of these tombs has the potential of helping to document and preserve these important historical structures. Issues concernng new and unique problems involving the photographing and digital reconstruction of these tombs are addressed. Techniques for removing image distortions, recovering 3-D shapes and correcting for lighting imbalances are discussed. A complete reconstruction of the tomb of Sennediem is shown.
文摘Abstract: This paper discusses the distribution pattern and geological significance of the carbon and oxygen isotopes (δ13C and δ18O) in the depositional sequences of Gaoyuzhuangian, Yangzhuangian and Wumishanian ages of the established Middle and Upper Proterozoic sequence stratigraphic framework in the Ming Tombs area lying in western Yanshan Mountain of Beijing. Besides, sketchy determination of δ13C and δ18O was also performed for other formations and members. The analytical results show the following: under the condition of clear-water carbonate sediments, δ13C and δ18O, featuring smaller variation of δ13C but larger variation of δ18O, can well delineate the relative change of sea level, which reflects the difference of primary sedimentary settings; in the presence of terrigenous substances, δ13C values vary greatly while δ18O slightly; the carbon and oxygen isotopes show marked changes at sequence boundaries. Besides, particular patterns can be found in regard to the distribution of carbon and oxygen isotopes within the sequences.
文摘Built between 1368 and 1911, The Imperial Tombs of the Ming （1368- 1644） and Qing （1644-1911） dynaslies includes Xianling Tombs of theMing Dynast）. Eastern and Western Qing Tornbs, Xiaoling Tomb of the Ming Dynasty.
