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     The Himalayan in the central western part of Yunnan can be divided into 4 tectonic episodes. The magmatic intrusion of them indicates 2 thermal cycles and the high tide of volcanic eruption takes place after the magmatic intrusion.
     云南中西部喜马拉雅期分为 4个构造幕 ,其岩浆侵入活动反映两个热旋回 ,当岩浆侵入活动结束后才出现火山喷发高潮。
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     HOT
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     Metallogeny in Relation to Supercontinent
     超大陆旋回和成矿作用
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     DISCUSSIONS ABOUT SEQUENCE BOUNDARIES ON CARBONATE PLATFORMS
     层序与旋回
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     Calc-alkaline volcanic rocks of Jiande formation in the northwest of Zhejiang province wereformed by four cycles of volcanic activities and underwent many times of thermal events.
     浙西北晚侏罗世火山岩历经四次火山喷发旋回,经受了多次事件。
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  thermal cycle
The results show that with the increase in the rate of welding thermal cycle, the solid dissolution of precipitate prior to liquation decreases and the thickness of liquid film produced by constitutional liquation increases.
      
Higher heating rate inhibits the further melting of adjacent matrix and the solidification of liquid by liquid-to-γ mode in the subsequent thermal cycle.
      
Deviations from Parameters of Thermal Cycle of Electric-Arc Welding of 12Kh1MF Heat-Resistant Steel Detected in Magnetic Charact
      
The delay occurs at that temperature at which the transformation terminated in the preliminary thermal cycle and is 3 °C.
      
It was also noted that the modified version overestimated the increase in the SWC following summer rainfall, which was attributed to an inadequate representation of the ground water and thermal cycle.
      
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The comprehensive results of whole-rock Sm-Nd and Rb-Sr and single grain zircon Pb-Pb dating suggest that the Qinling Group in the Qinling erogenic belt, northwestern Henan was formed at about 1200 Ma. The complex rocks in the interior of the erogenic belt experienced strong reworking in response to two great thermal cycles-the Jinning and the Caledonian cycles. Further disintegration of the Qinling Group delineated at present seems highly possible.

全岩Sm-Nd、Rb-Sr和单晶锆石~(207)Pb-~(206)Pb年代学的综合研究表明,豫西东秦岭造山带核部杂岩中的变质地层(秦岭群)大约在1200Ma形成;核部杂岩经历了晋宁旋回和加里东-海西旋回两个巨热旋回的影响与再造,目前划定的秦岭群仍有解体的可能性。

The polymetamorphic calcareous rocks of Qinling Complex in western Henan were intensively affected by both Jinninian Tectonothermal Cycle and Caledonian-Hercynian Tectonothermal Cycle. In the Jinning Cycle, the regional amphibolite-upper amphibolite facies metamorphism gave rise to three progressive metamorphic zones. The foresterite zone is distributed in the core, with the diopside zone and tremolite zone bordering on its south and north, respectively. The subsequent Caledonian-Hercynian Tectonothermal Cycle...

The polymetamorphic calcareous rocks of Qinling Complex in western Henan were intensively affected by both Jinninian Tectonothermal Cycle and Caledonian-Hercynian Tectonothermal Cycle. In the Jinning Cycle, the regional amphibolite-upper amphibolite facies metamorphism gave rise to three progressive metamorphic zones. The foresterite zone is distributed in the core, with the diopside zone and tremolite zone bordering on its south and north, respectively. The subsequent Caledonian-Hercynian Tectonothermal Cycle did not cause further growth of minerals throughout the region except for those rocks within the thermal aureole of some synchronous intrusive granites. In such an aureole in Shewei area, some nonequilibrium textures including corona,symplectite and exsolution lameller are well preserved in the calcareous rocks, which permits us to reconstruct the metamorphic reaction sequence of both prograde and retrograde processes and the P-T-X_(CO_2) trajectories during the cooling process. The prograde P-T path of the contact metamorphism is near isobaric heating; the metamorphic peak conditions are T≥750℃ and P=500~700MPa. The retrograde P-T path is near isobaric. In terms of the phase relationships from the thermodynamic calculated isobaric T-X_(CO_2) diagram, the X_(CO_2) for both carbonate rocks and meta-calcsilicate rocks decreased gradually with decrease of the metamorphic temperature.

秦岭杂岩中的钙质变质岩经历了晋宁和加里东-海西两个巨构造-热旋回的强烈影响和改造。在加里东的深位(≥15km)接触热变晕的钙质变质岩中,保存了若干精美的非平衡结构。凭借非平衡结构的研究分析,重塑了接触热变质的递进变质和退变质阶段的反应形式以及冷却过程的P-T-X_(co_2)路径。

There are two major metallogenic provinces of super large sedimentary hydrothermal sulfide ore deposits in North China:Langshan mountains and Qinling range,such as Changba Zn Pb deposits, Dongshengmiao Zn pyrite deposits et al Those ore deposits were formed by the hydrothermal convection system circulating through underlying sedimentary columns and the basement in the progressive heating stages of the thermal cycle during the transformation periods from tension to compression of the non active continental...

There are two major metallogenic provinces of super large sedimentary hydrothermal sulfide ore deposits in North China:Langshan mountains and Qinling range,such as Changba Zn Pb deposits, Dongshengmiao Zn pyrite deposits et al Those ore deposits were formed by the hydrothermal convection system circulating through underlying sedimentary columns and the basement in the progressive heating stages of the thermal cycle during the transformation periods from tension to compression of the non active continental margins

中国北方超大型热水沉积硫化物矿床成矿模式李英祁思敬(西安地质学院,西安710054)关键词超大型矿床热水沉积作用大陆边缘盆地热旋回中国北方超大型热水沉积硫化物矿床(SEDEX)集中产出于华北地台北缘西段与扬子地台北缘西段,即秦岭与狼山两区。可确定的矿...

 
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