Based on the concept of "active blocks" and spatial distribution of historical earthquakes with surface ruptures as well as major and subordinate active faults. The Sichuan-Yunnan region can be divided into ...Based on the concept of "active blocks" and spatial distribution of historical earthquakes with surface ruptures as well as major and subordinate active faults. The Sichuan-Yunnan region can be divided into four first-order blocks. They are the Markam block (I), the Sichuan-Yunnan rhombic block (II), Baoshan-Pu'er block (III), and Mizhina-Ximeng block (IV). Cut by sub-ordinate NE-trending active faults, the Sichuan-Yunnan rhombic block (II) can be further divided into two sub-blocks: the northwestern Sichuan sub-block (II1) and the middle Yunnan sub-block (II2), while the Baoshan- Pu'er block (III) can be further divided into three sub-blocks: Baoshan sub-block (III1), Jinggu sub-block (III2), and Mengla sub-block (III3). A quantitative study of offset landforms is carried out and the basic types of active faults and their long-term slip rates along the major boundaries of active blocks of different orders in the Sichuan-Yunnan region are determined, through slip vector analysis, the motion states of the active blocks are clarified and the deformation coordination on the block margins is discussed. It is suggested that the tectonic motion of the blocks in this region is a complex or superimposition of three basic types of motions: southeastward sliding, rotating on vertical axis, and uplifting. The Markam block (I), the northwestern Sichuan sub-block (II1), and middle Yunnan sub-block (II2) have a southeastward horizontal sliding rate of 1-5 mm/a, clockwise rotating angular rate of 1.4-4(/Ma, and uplifting rate of about 1 mm/a. The Baoshan-Pu'er (III) and Mizhina-Ximeng (IV) blocks have also been extensively clockwise rotated. This pattern of motion is a strain response to the collision between the Indian and Eurasian plates and the localized deformation and differential slip on the block margins associated with the northward motion of the Indian Plate. Because a set of transverse thrusts between the blocks absorbs and transforms some components of eastward or southeastward sliding motion, the eastward escape or 展开更多
文摘Based on the concept of "active blocks" and spatial distribution of historical earthquakes with surface ruptures as well as major and subordinate active faults. The Sichuan-Yunnan region can be divided into four first-order blocks. They are the Markam block (I), the Sichuan-Yunnan rhombic block (II), Baoshan-Pu'er block (III), and Mizhina-Ximeng block (IV). Cut by sub-ordinate NE-trending active faults, the Sichuan-Yunnan rhombic block (II) can be further divided into two sub-blocks: the northwestern Sichuan sub-block (II1) and the middle Yunnan sub-block (II2), while the Baoshan- Pu'er block (III) can be further divided into three sub-blocks: Baoshan sub-block (III1), Jinggu sub-block (III2), and Mengla sub-block (III3). A quantitative study of offset landforms is carried out and the basic types of active faults and their long-term slip rates along the major boundaries of active blocks of different orders in the Sichuan-Yunnan region are determined, through slip vector analysis, the motion states of the active blocks are clarified and the deformation coordination on the block margins is discussed. It is suggested that the tectonic motion of the blocks in this region is a complex or superimposition of three basic types of motions: southeastward sliding, rotating on vertical axis, and uplifting. The Markam block (I), the northwestern Sichuan sub-block (II1), and middle Yunnan sub-block (II2) have a southeastward horizontal sliding rate of 1-5 mm/a, clockwise rotating angular rate of 1.4-4(/Ma, and uplifting rate of about 1 mm/a. The Baoshan-Pu'er (III) and Mizhina-Ximeng (IV) blocks have also been extensively clockwise rotated. This pattern of motion is a strain response to the collision between the Indian and Eurasian plates and the localized deformation and differential slip on the block margins associated with the northward motion of the Indian Plate. Because a set of transverse thrusts between the blocks absorbs and transforms some components of eastward or southeastward sliding motion, the eastward escape or
文摘研究茬口对轮作作物的产量贡献及干物质积累与分配规律的影响,对于优化作物高产高效栽培理论和技术具有重要意义。本研究在甘肃河西绿洲灌区,通过田间试验,研究了前茬小麦不同秸秆还田方式（25 cm高茬收割免耕,NTSS;25 cm高茬等量秸秆覆盖免耕,NTS;25 cm高茬等量秸秆翻压,TIS;低茬收割翻耕,CT）对轮作玉米干物质积累和分配及产量的影响,以期为该区前茬小麦轮作玉米生产模式提供优化依据。结果表明,与CT相比,NTSS、NTS、TIS提高了玉米抽穗后干物质的积累量,两年平均高4.8%~12.7%,NTS较NTSS、TIS具有更高的干物质累积作用;NTSS、NTS、TIS可提高玉米叶、茎、鞘对籽粒的贡献率,提高幅度平均为12.8%~25.0%、6.3%~11.3%、18.3%~78.4%,其中NTS较NTSS、TIS提高作用更突出。NTSS、NTS、TIS提高了玉米的籽粒产量,增幅为11.3%~17.5%,其中NTS两年籽粒产量最高,分别达到13 470 kg hm–2和13 274 kg hm–2,较TIS高5.6%~9.0%;穗粒数增加是小麦秸秆还田提高轮作玉米产量的主要原因。同时NTS获得较高的收获指数,提高比例为6.4%~8.4%,说明NTS较其他处理增产的另一原因是提高了收获指数。本研究表明,其前茬小麦秸秆覆盖结合免耕（NTS）可作为绿洲灌区优化后茬玉米干物质累积规律及获得高产的理想耕作措施。
