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| 1 | Prediction of in situ degrada- tion characteristics of neutral detergent fibre (aNDF) in temper- ate grasses and red clover using near-infrared reflectance spectros- copy (NIRS)显示文摘 | Hege N Harald V Gustav F | 2007 | Anita Feed Sci Tech2007，139，1： | 1 |
| 2 | Percutaneous ethanol injection therapy in the treatment of thyroid and parathyroid diseases 显示文摘 | Bennedbaek F N Karstrup S Hegedüs L | 1997 | Eur J Endocrinol1997，136，3： | 1 |
| 3 | Percutaneous ethanol injection therapy in benign solitary solid cold thyroid nodules: a randomized trial comparing one injection with three injections 显示文摘 | Bennedbaek F N Hegedüs L | 1999 | Thyroid1999，9，3： | 1 |
| 4 | Effect of percutaneous ethanol injection therapy versus suppressive doses of L-thyroxine on benign solitary solid cold thyroid nodules: a randomized trial 显示文摘 | Bennedbaek F N Nielsen L K Hegedüs L | 1998 | J Clin Endocrinol Metab1998，83，3： | 1 |
| 5 | Application of the 5'-nuclease PCR assay in evaluation and development of methods for quantitative detection campylobacter jejuni 显示文摘 | Hege K N Anette B Knut Rudi | 2000 | Appl Environ Micobiol2000，66，9： | 1 |
| 6 | Origin of overpres sures in shales: Constraints from basin modeling显示文摘 | Hege M N B Christian H Gunn M D T | 2004 | AAPG Bulletin2004，88，2： | 1 |
| 7 | 利用被动源地震实验和接收函数分析确定迪纳拉山脉北部和潘诺尼亚盆地西南部交界处地壳结构显示文摘通过在迪纳拉山脉和潘诺尼亚盆地西南交界带进行被动源地震实验,确定了地壳结构和波速不连续面。实验目的是确定亚得里亚海微板块与作为欧洲板块一部分的潘诺尼亚地块的关系。大部分流动台站沿着Alp07剖面(主动源ALP 2002项目的一部分)布设在克罗地亚。该剖面从伊斯特拉半岛到德拉瓦河沿线呈西西南-东东南向延伸约300km。利用P波接收函数方法分析测线上13个临时地震台站的远震记录。Alp07剖面得到了两种特征接收函数(RF),分属于迪纳拉和潘诺尼亚地壳,交界带则包含两种类型。迪纳拉型地壳主要包含三组地壳不连续面:沉积基底、壳内不连续面和莫霍不连续面,而潘诺尼亚类型地壳仅包含两组不连续界面。在潘诺尼亚型地壳中并未观测到壳内不连续面,因此认为潘诺尼亚盆地为单层地壳结构。应用接收函数正演模拟和H-κ叠加两种分析方法开展了地壳结构研究,并将该结果与Alp07剖面主动源折射地震结果进行了比较。接收函数模拟得到了可靠的莫霍面深度结果,与Alp07剖面的地震折射结果相一致,即潘诺尼亚区域地壳特征为简单地壳结构,波速较低(VP在5.9~6.2km/s)。迪纳拉及其周缘,由于地壳结构更为复杂,接收函数模拟得到莫霍面深度较Alp07剖面更大,高达15%。受短周期台站数据频带限制,利用H-κ叠加方法计算得到的莫霍面深度在较大范围内(±13km)变化。通过与先前所有结果进行对比,排除了差异较大的5个台站的结果,而与Alp07剖面附近的莫霍不连续面相比,其他7个台站莫霍面深度差异在15%内变化。 | Franjo umanovac Endre Hegedüs Jasna Oreskovi Sasa Kolar Attila C.Kovcs Darko Dudjak Istvn J.Kovcs 王林 | 2017 | 世界地震译丛2017，48，1： | 0 |
| 8 | A Comparison of the Genetic Shaft Types of Some Karst Areas Based on Their Specific Shaft Lengths显示文摘Shaft development can be documented on the basis of comparative studies of specific shaft lengths and shaft patterns.We calculated the specific length of shafts and the average specific shaft length of the shafts in some karst areas and we investigated the relation between the altitude of shaft floors and the specific shaft length.Taking the registered specific shaft lengths and the shaft patterns into consideration,it can be stated that some parts of the shafts developed paragenetically in the studied karst areas.In the Bakony Region,this was caused by surface water influx,rise of karst water level,and their simultaneous effect.As a result,shaft systems,bifurcating shafts and storeyed shafts developed.On glaciokarst areas,shafts may constitute a system with phreatic passages:either because a phreatic environment developed in the vadose zone due to the permanent impoundment of karst water or because a phreatic passage got into the vadose zone since the karst became elevated.On the studied karst areas,the following shaft development types are distinguished:glacial-high mountain surface flood development type(1),glacial-high mountain karst water and surface flood development type(2),glacial karst water and surface flood later phreatic development type(3),shaft with a passage that got into the vadose zone(4). | Márton Veress András Hegedűs Pavle Cikovac Ruban Dmitry A Kálmán Péntek | 2019 | Journal of Geological Research2019，1，3： | 0 |
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