目的调查家人参与患者的康复训练及心理支持治疗能否改善患者日常生活能力及患者焦虑抑郁状态。方法选取脑卒中恢复期的患者120例,随机分为对照组(61例)和治疗组(59例),对照组仅接受约2周的住院康复治疗,治疗组除了接受2周的住院康复治...目的调查家人参与患者的康复训练及心理支持治疗能否改善患者日常生活能力及患者焦虑抑郁状态。方法选取脑卒中恢复期的患者120例,随机分为对照组(61例)和治疗组(59例),对照组仅接受约2周的住院康复治疗,治疗组除了接受2周的住院康复治疗外,居家后接受家人康复训练和心理支持治疗,主要结局为90 d的改良Rankin量表(modified Rankin scale,mRS)0~2分的比率,次要结局为90 d的mRS 0~3分的比率,90 d FuglMeyer评分增加值,90 d Barthel评分改善值以及90 d抑郁自评量表分下降值。结果治疗组和对照组90 d mRS 0~2分占比分别为55.9%、36.1%,差异有统计学意义,两组mRS 0~3分的比率差异有统计学意义。治疗组90 d FuglMeyer、Barthel评分改善高于对照组,差异有统计学意义。两组90 d时抑郁自评量表评分下降分值为4(0,5)、2(0,6),差异具有统计学意义。结论培训家人对急性缺血性卒中患者进行康复训练,同时辅助家人对患者进行心理疏导能够改善患者3个月时的日常生活能力,减轻患者抑郁状态。展开更多
Mesoproterozoic volcanic rocks occurring in the north of the western Kunlun Mountains can be divided into two groups. The first group (north belt) is an reversely-evolved bimodal series. Petrochemistry shows that the ...Mesoproterozoic volcanic rocks occurring in the north of the western Kunlun Mountains can be divided into two groups. The first group (north belt) is an reversely-evolved bimodal series. Petrochemistry shows that the alkalinity of the rocks decreases from early to late: alkaline→calc-alkaline→tholeiite, and geochemistry proves that the volcanic rocks were formed in rifting tectonic systems. The sedimentary facies shows characteristics of back-arc basins. The second (south belt) group, which occurs to the south of Yutian-Minfeng-Cele, is composed of calc-alkaline island arc (basaltic) andesite and minor rhyolite. The space distribution, age and geochemistry of the two volcanite groups indicate that they were formed in a back-arc basin (the first group) and an island arc (the second group) respectively and indicate the plate evolution during the Mesoproterozoic. The orogeny took place at -1.05 Ga, which was coeval with the Grenville orogeny. This study has provided important geological data for exploring the position of the Paleo-Tarim plate in the Rodinia super-continent.展开更多
The West Kunlun ore-forming belt is located between the northwestern Qinghai-Tibet Plateau and southwestern Tarim Basin. It situated between the Paleo-Asian Tectonic Domain and Tethyan Tectonic Domain. It is an import...The West Kunlun ore-forming belt is located between the northwestern Qinghai-Tibet Plateau and southwestern Tarim Basin. It situated between the Paleo-Asian Tectonic Domain and Tethyan Tectonic Domain. It is an important component of the giant tectonic belt in central China (the Kunlun-Qilian-Qinling Tectonic Belt or the Central Orogenic Belt). Many known ore-forming belts such as the Kunlun-Qilian Qinling ore-forming zone, Sanjiang (or Three river) ore-forming zone, Central Asian ore-forming zone, etc. pass through the West Kunlun area. Three ore-forming zones and seven ore-forming subzones were classified, and eighteen mineralization areas were marked. It is indicated that the West Kunlun area is one of the most favorable region for finding out large and superlarge ore deposits.展开更多
文摘目的调查家人参与患者的康复训练及心理支持治疗能否改善患者日常生活能力及患者焦虑抑郁状态。方法选取脑卒中恢复期的患者120例,随机分为对照组(61例)和治疗组(59例),对照组仅接受约2周的住院康复治疗,治疗组除了接受2周的住院康复治疗外,居家后接受家人康复训练和心理支持治疗,主要结局为90 d的改良Rankin量表(modified Rankin scale,mRS)0~2分的比率,次要结局为90 d的mRS 0~3分的比率,90 d FuglMeyer评分增加值,90 d Barthel评分改善值以及90 d抑郁自评量表分下降值。结果治疗组和对照组90 d mRS 0~2分占比分别为55.9%、36.1%,差异有统计学意义,两组mRS 0~3分的比率差异有统计学意义。治疗组90 d FuglMeyer、Barthel评分改善高于对照组,差异有统计学意义。两组90 d时抑郁自评量表评分下降分值为4(0,5)、2(0,6),差异具有统计学意义。结论培训家人对急性缺血性卒中患者进行康复训练,同时辅助家人对患者进行心理疏导能够改善患者3个月时的日常生活能力,减轻患者抑郁状态。
文摘Mesoproterozoic volcanic rocks occurring in the north of the western Kunlun Mountains can be divided into two groups. The first group (north belt) is an reversely-evolved bimodal series. Petrochemistry shows that the alkalinity of the rocks decreases from early to late: alkaline→calc-alkaline→tholeiite, and geochemistry proves that the volcanic rocks were formed in rifting tectonic systems. The sedimentary facies shows characteristics of back-arc basins. The second (south belt) group, which occurs to the south of Yutian-Minfeng-Cele, is composed of calc-alkaline island arc (basaltic) andesite and minor rhyolite. The space distribution, age and geochemistry of the two volcanite groups indicate that they were formed in a back-arc basin (the first group) and an island arc (the second group) respectively and indicate the plate evolution during the Mesoproterozoic. The orogeny took place at -1.05 Ga, which was coeval with the Grenville orogeny. This study has provided important geological data for exploring the position of the Paleo-Tarim plate in the Rodinia super-continent.
文摘The West Kunlun ore-forming belt is located between the northwestern Qinghai-Tibet Plateau and southwestern Tarim Basin. It situated between the Paleo-Asian Tectonic Domain and Tethyan Tectonic Domain. It is an important component of the giant tectonic belt in central China (the Kunlun-Qilian-Qinling Tectonic Belt or the Central Orogenic Belt). Many known ore-forming belts such as the Kunlun-Qilian Qinling ore-forming zone, Sanjiang (or Three river) ore-forming zone, Central Asian ore-forming zone, etc. pass through the West Kunlun area. Three ore-forming zones and seven ore-forming subzones were classified, and eighteen mineralization areas were marked. It is indicated that the West Kunlun area is one of the most favorable region for finding out large and superlarge ore deposits.
